Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa
The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Neverthele...
Ausführliche Beschreibung
Autor*in: |
Kütter, Sissy - 1983- [verfasserIn] |
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Hochschulschrift: |
Dissertation ; Universität Potsdam ; 2015 |
Format: |
E-Book |
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Sprache: |
Englisch |
Erschienen: |
Potsdam: 2015 |
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Schlagwörter: |
Barberton Greenstone Belt / Grünstein / Metabasit / Magnetotellurik / Elektromagnetische Messung / Elektromagnetisches Verfahren Südafrika / Archaikum, Geologie / Grünsteingürtel / Tiefenstruktur, Geologie / Elektromagnetische Tiefensondierung / Elektrische Leitfähigkeit Datenanalyse / Datenauswertung / Störsignal / Filter, Mathematik / Methode |
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Formangabe: |
Hochschulschrift |
Umfang: |
1 Online-Ressource (xix, 156 Seiten) ; Illustrationen, Diagramme, Karten |
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Weitere Ausgabe: |
Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 -: Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa - 2015 Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 -: Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa - Potsdam, 2015 |
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Links: |
Link aufrufen |
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DOI / URN: |
urn:nbn:de:kobv:517-opus4-83198 |
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Katalog-ID: |
857554905 |
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245 | 1 | 0 | |a Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa |c vorgelegt von Diplom-Geophysikerin Sissy Kütter |
246 | 3 | 3 | |a Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika |
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520 | |a The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. | ||
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Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa vorgelegt von Diplom-Geophysikerin Sissy Kütter |
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magnetotelluric measurements across the southern barberton greenstone belt, south africa |
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Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa |
abstract |
The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. |
abstractGer |
The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. |
abstract_unstemmed |
The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. |
url |
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Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. 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1218399805 DE-101 urn:nbn:de:kobv:517-opus4-83198 urn (DE-627)857554905 (DE-576)470455748 (DE-599)GBV857554905 (OCoLC)947944967 (OCoLC)953267773 DE-627 ger DE-627 rda eng XA-DE-BB XA-DE 551.8 DE-101 550 DE-101 38.71 bkl 38.55 bkl Kütter, Sissy 1983- verfasserin (DE-588)1098339185 (DE-627)857551809 (DE-576)469079622 aut Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa vorgelegt von Diplom-Geophysikerin Sissy Kütter Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika Potsdam 2015 1 Online-Ressource (xix, 156 Seiten) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Potsdam 2015 The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4589361-5 (DE-627)325955743 (DE-576)214014967 Barberton Greenstone Belt gnd s (DE-588)4338549-7 (DE-627)15241181X (DE-576)211389528 Grünstein gnd s (DE-588)4254969-3 (DE-627)104660090 (DE-576)210543620 Metabasit gnd s (DE-588)4168603-2 (DE-627)104346337 (DE-576)209916826 Magnetotellurik gnd s (DE-588)4342450-8 (DE-627)153371684 (DE-576)211433292 Elektromagnetische Messung gnd s (DE-588)4529179-2 (DE-627)254346790 (DE-576)213378574 Elektromagnetisches Verfahren gnd DE-101 g (DE-588)4078012-0 (DE-627)106078739 (DE-576)209206934 Südafrika gnd s (DE-588)4278975-8 (DE-627)104167548 (DE-576)210740345 Archaikum Geologie gnd s (DE-588)4346895-0 (DE-627)156887940 (DE-576)211479306 Grünsteingürtel gnd s (DE-588)4483774-4 (DE-627)23912247X (DE-576)21290745X Tiefenstruktur Geologie gnd s (DE-588)4470959-6 (DE-627)234861134 (DE-576)212775014 Elektromagnetische Tiefensondierung gnd s (DE-588)4014200-0 (DE-627)106340859 (DE-576)208906924 Elektrische Leitfähigkeit gnd DE-101 s (DE-588)4123037-1 (DE-627)105758051 (DE-576)209556331 Datenanalyse gnd s (DE-588)4131193-0 (DE-627)105696773 (DE-576)20962535X Datenauswertung gnd s (DE-588)4210217-0 (DE-627)105098213 (DE-576)210196807 Störsignal gnd s (DE-588)4154388-9 (DE-627)105523828 (DE-576)209810831 Filter Mathematik gnd s (DE-588)4038971-6 (DE-627)106230158 (DE-576)209032642 Methode gnd DE-101 Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 - Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa 2015 xix, 156 Seiten (DE-627)1620059649 (DE-576)470455489 Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 - Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa Potsdam, 2015 xix, 156 Seiten (DE-627)857543946 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 Resolving-System kostenfrei Volltext https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docld/8319 Verlag Volltext kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-83198 2020-10-07 Resolving-System https://d-nb.info/1218399805/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/8319 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER Blocktest 38.71 Geomagnetik Geoelektrik Geothermie SEPA (DE-627)106407228 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 551.8 20 01 0084 3782404009 x 20-10-20 21 01 0046 3782443349 z 20-10-20 22 01 0018 3782482468 SUBolrd xu 20-10-20 23 01 0830 3782521765 olr-d x 20-10-20 30 01 0104 3782545494 z 20-10-20 40 01 0007 3782566254 xsn 20-10-20 60 01 0705 3782604512 OLRD z 20-10-20 63 01 3401 3782643402 ORD x 20-10-20 65 01 0003 4167690039 GBV-ODiss Open Access z 16-07-22 70 01 0089 3782662717 zdo 20-10-20 105 01 0841 3782869168 z 20-10-20 110 01 3110 3782686896 x 20-10-20 132 01 0959 3782712218 OLR-DISS x 20-10-20 151 01 0546 3782751086 OLR-ODISS z 20-10-20 161 01 0960 3782765230 ORD z 20-10-20 285 01 0517 1612095992 00 9300 --%%-- s --%%-- z 27-04-16 293 01 3293 3782840763 ORD z 20-10-20 370 01 4370 3782866029 x 20-10-20 2027 01 DE-105 3392782157 00 --%%-- --%%-- n --%%-- l01 08-06-16 2403 01 DE-LFER 3392782327 00 --%%-- --%%-- n --%%-- l01 14-06-16 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 285 01 0517 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TG 3200 285 00 DE-517 00 TG 03100 2027 01 DE-105 00 (DE-627)1292105569 DK 550.837.6 2027 01 DE-105 01 (DE-627)1292244216 DK 550.8.05 2027 01 DE-105 02 (DE-627)129403703X DK 552.323 2027 01 DE-105 03 (DE-627)1294037048 DK 551.71 2027 01 DE-105 04 (DE-627)130101639X DK 916.825 2027 01 DE-105 05 (DE-627)129278105X DK 378.245 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-10-20:01:13:43 |
allfields_unstemmed |
1218399805 DE-101 urn:nbn:de:kobv:517-opus4-83198 urn (DE-627)857554905 (DE-576)470455748 (DE-599)GBV857554905 (OCoLC)947944967 (OCoLC)953267773 DE-627 ger DE-627 rda eng XA-DE-BB XA-DE 551.8 DE-101 550 DE-101 38.71 bkl 38.55 bkl Kütter, Sissy 1983- verfasserin (DE-588)1098339185 (DE-627)857551809 (DE-576)469079622 aut Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa vorgelegt von Diplom-Geophysikerin Sissy Kütter Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika Potsdam 2015 1 Online-Ressource (xix, 156 Seiten) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Potsdam 2015 The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4589361-5 (DE-627)325955743 (DE-576)214014967 Barberton Greenstone Belt gnd s (DE-588)4338549-7 (DE-627)15241181X (DE-576)211389528 Grünstein gnd s (DE-588)4254969-3 (DE-627)104660090 (DE-576)210543620 Metabasit gnd s (DE-588)4168603-2 (DE-627)104346337 (DE-576)209916826 Magnetotellurik gnd s (DE-588)4342450-8 (DE-627)153371684 (DE-576)211433292 Elektromagnetische Messung gnd s (DE-588)4529179-2 (DE-627)254346790 (DE-576)213378574 Elektromagnetisches Verfahren gnd DE-101 g (DE-588)4078012-0 (DE-627)106078739 (DE-576)209206934 Südafrika gnd s (DE-588)4278975-8 (DE-627)104167548 (DE-576)210740345 Archaikum Geologie gnd s (DE-588)4346895-0 (DE-627)156887940 (DE-576)211479306 Grünsteingürtel gnd s (DE-588)4483774-4 (DE-627)23912247X (DE-576)21290745X Tiefenstruktur Geologie gnd s (DE-588)4470959-6 (DE-627)234861134 (DE-576)212775014 Elektromagnetische Tiefensondierung gnd s (DE-588)4014200-0 (DE-627)106340859 (DE-576)208906924 Elektrische Leitfähigkeit gnd DE-101 s (DE-588)4123037-1 (DE-627)105758051 (DE-576)209556331 Datenanalyse gnd s (DE-588)4131193-0 (DE-627)105696773 (DE-576)20962535X Datenauswertung gnd s (DE-588)4210217-0 (DE-627)105098213 (DE-576)210196807 Störsignal gnd s (DE-588)4154388-9 (DE-627)105523828 (DE-576)209810831 Filter Mathematik gnd s (DE-588)4038971-6 (DE-627)106230158 (DE-576)209032642 Methode gnd DE-101 Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 - Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa 2015 xix, 156 Seiten (DE-627)1620059649 (DE-576)470455489 Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 - Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa Potsdam, 2015 xix, 156 Seiten (DE-627)857543946 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 Resolving-System kostenfrei Volltext https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docld/8319 Verlag Volltext kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-83198 2020-10-07 Resolving-System https://d-nb.info/1218399805/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/8319 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER Blocktest 38.71 Geomagnetik Geoelektrik Geothermie SEPA (DE-627)106407228 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 551.8 20 01 0084 3782404009 x 20-10-20 21 01 0046 3782443349 z 20-10-20 22 01 0018 3782482468 SUBolrd xu 20-10-20 23 01 0830 3782521765 olr-d x 20-10-20 30 01 0104 3782545494 z 20-10-20 40 01 0007 3782566254 xsn 20-10-20 60 01 0705 3782604512 OLRD z 20-10-20 63 01 3401 3782643402 ORD x 20-10-20 65 01 0003 4167690039 GBV-ODiss Open Access z 16-07-22 70 01 0089 3782662717 zdo 20-10-20 105 01 0841 3782869168 z 20-10-20 110 01 3110 3782686896 x 20-10-20 132 01 0959 3782712218 OLR-DISS x 20-10-20 151 01 0546 3782751086 OLR-ODISS z 20-10-20 161 01 0960 3782765230 ORD z 20-10-20 285 01 0517 1612095992 00 9300 --%%-- s --%%-- z 27-04-16 293 01 3293 3782840763 ORD z 20-10-20 370 01 4370 3782866029 x 20-10-20 2027 01 DE-105 3392782157 00 --%%-- --%%-- n --%%-- l01 08-06-16 2403 01 DE-LFER 3392782327 00 --%%-- --%%-- n --%%-- l01 14-06-16 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 285 01 0517 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TG 3200 285 00 DE-517 00 TG 03100 2027 01 DE-105 00 (DE-627)1292105569 DK 550.837.6 2027 01 DE-105 01 (DE-627)1292244216 DK 550.8.05 2027 01 DE-105 02 (DE-627)129403703X DK 552.323 2027 01 DE-105 03 (DE-627)1294037048 DK 551.71 2027 01 DE-105 04 (DE-627)130101639X DK 916.825 2027 01 DE-105 05 (DE-627)129278105X DK 378.245 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-10-20:01:13:43 |
allfieldsGer |
1218399805 DE-101 urn:nbn:de:kobv:517-opus4-83198 urn (DE-627)857554905 (DE-576)470455748 (DE-599)GBV857554905 (OCoLC)947944967 (OCoLC)953267773 DE-627 ger DE-627 rda eng XA-DE-BB XA-DE 551.8 DE-101 550 DE-101 38.71 bkl 38.55 bkl Kütter, Sissy 1983- verfasserin (DE-588)1098339185 (DE-627)857551809 (DE-576)469079622 aut Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa vorgelegt von Diplom-Geophysikerin Sissy Kütter Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika Potsdam 2015 1 Online-Ressource (xix, 156 Seiten) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Potsdam 2015 The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. 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1218399805 DE-101 urn:nbn:de:kobv:517-opus4-83198 urn (DE-627)857554905 (DE-576)470455748 (DE-599)GBV857554905 (OCoLC)947944967 (OCoLC)953267773 DE-627 ger DE-627 rda eng XA-DE-BB XA-DE 551.8 DE-101 550 DE-101 38.71 bkl 38.55 bkl Kütter, Sissy 1983- verfasserin (DE-588)1098339185 (DE-627)857551809 (DE-576)469079622 aut Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa vorgelegt von Diplom-Geophysikerin Sissy Kütter Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika Potsdam 2015 1 Online-Ressource (xix, 156 Seiten) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Potsdam 2015 The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB. 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Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa 2015 xix, 156 Seiten (DE-627)1620059649 (DE-576)470455489 Erscheint auch als Druck-Ausgabe Kütter, Sissy, 1983 - Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa Potsdam, 2015 xix, 156 Seiten (DE-627)857543946 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 Resolving-System kostenfrei Volltext https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docld/8319 Verlag Volltext kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-83198 2020-10-07 Resolving-System https://d-nb.info/1218399805/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/8319 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER Blocktest 38.71 Geomagnetik Geoelektrik Geothermie SEPA (DE-627)106407228 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 551.8 20 01 0084 3782404009 x 20-10-20 21 01 0046 3782443349 z 20-10-20 22 01 0018 3782482468 SUBolrd xu 20-10-20 23 01 0830 3782521765 olr-d x 20-10-20 30 01 0104 3782545494 z 20-10-20 40 01 0007 3782566254 xsn 20-10-20 60 01 0705 3782604512 OLRD z 20-10-20 63 01 3401 3782643402 ORD x 20-10-20 65 01 0003 4167690039 GBV-ODiss Open Access z 16-07-22 70 01 0089 3782662717 zdo 20-10-20 105 01 0841 3782869168 z 20-10-20 110 01 3110 3782686896 x 20-10-20 132 01 0959 3782712218 OLR-DISS x 20-10-20 151 01 0546 3782751086 OLR-ODISS z 20-10-20 161 01 0960 3782765230 ORD z 20-10-20 285 01 0517 1612095992 00 9300 --%%-- s --%%-- z 27-04-16 293 01 3293 3782840763 ORD z 20-10-20 370 01 4370 3782866029 x 20-10-20 2027 01 DE-105 3392782157 00 --%%-- --%%-- n --%%-- l01 08-06-16 2403 01 DE-LFER 3392782327 00 --%%-- --%%-- n --%%-- l01 14-06-16 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 285 01 0517 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-83198 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TG 3200 285 00 DE-517 00 TG 03100 2027 01 DE-105 00 (DE-627)1292105569 DK 550.837.6 2027 01 DE-105 01 (DE-627)1292244216 DK 550.8.05 2027 01 DE-105 02 (DE-627)129403703X DK 552.323 2027 01 DE-105 03 (DE-627)1294037048 DK 551.71 2027 01 DE-105 04 (DE-627)130101639X DK 916.825 2027 01 DE-105 05 (DE-627)129278105X DK 378.245 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-10-20:01:13:43 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a22002652 4500</leader><controlfield tag="001">857554905</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230108230445.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">160608s2015 gw |||||om 00| ||eng c</controlfield><datafield tag="016" ind1="7" ind2=" "><subfield code="a">1218399805</subfield><subfield code="2">DE-101</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">urn:nbn:de:kobv:517-opus4-83198</subfield><subfield code="2">urn</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)857554905</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-576)470455748</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBV857554905</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)947944967</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)953267773</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE-BB</subfield><subfield code="c">XA-DE</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">551.8</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.71</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.55</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kütter, Sissy</subfield><subfield code="d">1983-</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(DE-588)1098339185</subfield><subfield code="0">(DE-627)857551809</subfield><subfield code="0">(DE-576)469079622</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa</subfield><subfield code="c">vorgelegt von Diplom-Geophysikerin Sissy Kütter</subfield></datafield><datafield tag="246" ind1="3" ind2="3"><subfield code="a">Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Potsdam</subfield><subfield code="c">2015</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (xix, 156 Seiten)</subfield><subfield code="b">Illustrationen, Diagramme, Karten</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Universität Potsdam</subfield><subfield code="d">2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Barberton Greenstone Belt (BGB) in the northwestern part of South Africa belongs to the few well-preserved remnants of Archean crust. Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB.</subfield></datafield><datafield tag="655" ind1=" " ind2="7"><subfield code="a">Hochschulschrift</subfield><subfield code="0">(DE-588)4113937-9</subfield><subfield code="0">(DE-627)105825778</subfield><subfield code="0">(DE-576)209480580</subfield><subfield code="2">gnd-content</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="D">g</subfield><subfield code="0">(DE-588)4589361-5</subfield><subfield code="0">(DE-627)325955743</subfield><subfield code="0">(DE-576)214014967</subfield><subfield code="a">Barberton Greenstone Belt</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="D">s</subfield><subfield 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ddc 551.8 ddc 550 bkl 38.71 bkl 38.55 gnd Barberton Greenstone Belt gnd Grünstein gnd Metabasit gnd Magnetotellurik gnd Elektromagnetische Messung gnd Elektromagnetisches Verfahren gnd Südafrika gnd Archaikum gnd Grünsteingürtel gnd Tiefenstruktur gnd Elektromagnetische Tiefensondierung gnd Elektrische Leitfähigkeit gnd Datenanalyse gnd Datenauswertung gnd Störsignal gnd Filter gnd Methode 2027 ebook |
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Magnetotelluric measurements across the southern Barberton Greenstone Belt, South Africa |
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Kütter, S. Kütter, Sissy Hochschulschrift Südafrika / Barberton Greenstone Belt Barberton Greenstone Belt Greenstone Grünstein Metabasit Magnetotellurik Elektromagnetische Messung Elektromagnetische Methode Elektromagnetisches Verfahren Zuid-Afrikaansche Republiek Republiek van Suid-Afrika Suidafrika Union von Südafrika Suid Africa Südafrikanische Republik Unie van Zuid-Africa South African Republic Suid-Afrika Azania Republik Südafrika Südafrikanische Union South Africa Republiek van Suidafrika Unie van Suid-Afrika ZAR (abku) Riphabulika ya Afurika Tshipembe Zuid-Africa Zuidafrikaansche Republiek Repaboliki ya Aferika Borwa Union of South Africa Republic of South Africa Südafrika Archäikum Altpräkambrium Archaikum <Geologie> Greenstone belt Grünsteingürtel Tiefenstruktur <Geologie> Elektromagnetische Tiefensondierung Konduktivität Äquivalentleitfähigkeit Elektrische Leitfähigkeit Data-analysis Statistische Auswertung Statistische Datenanalyse Data analysis Datenauswertung <Statistik> Datenanalyse Datenauswertung Störsignal Mathematisches Filter Filter <Mathematik> Technik <Methode> Verfahren <Methode> Methoden Methodik Methode Bostanium Postampium Poztupimi Potzdam Bostampium Potsdamum State Capital of Potsdam Stadtgemeinde Potsdam Residenzstadt Potsdam Potestampium Potsdam-Sanssouci Pozdam Potsdamm Landeshauptstadt Potsdam Potsdam |
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Magnetotellurische Messungen am südlichen Barberton Grünsteingürtel, Südafrika |
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Over the last centuries, the BGB has been intensively studied at surface with detailed mapping of its surfacial geological units and tectonic features. Nevertheless, the deeper structure of the BGB remains poorly understood. Various tectonic evolution models have been developed based on geo-chronological and structural data. These theories are highly controversial and centre on the question whether plate tectonics - as geoscientists understand them today - was already evolving on the Early Earth or whether vertical mass movements driven by the higher temperature of the Earth in Archean times governed continent development. To get a step closer to answering the questions regarding the internal structure and formation of the BGB, magnetotelluric (MT) field experiments were conducted as part of the German-South African research initiative Inkaba yeAfrica. Five-component MT data (three magnetic and two electric channels) were collected at ~200 sites aligned along six profiles crossing the southern part of the BGB. Tectonic features like (fossil) faults and shear zones are often mineralized and therefore can have high electrical conductivities. Hence, by obtaining an image of the conductivity distribution of the subsurface from MT measurements can provide useful information on tectonic processes. Unfortunately, the BGB MT data set is heavily affected by man-made electromagnetic noise caused, e.g. by powerlines and electric fences. Aperiodic spikes in the magnetic and corresponding offsets in the electric field components impair the data quality particularly at periods >1 s which are required to image deep electrical structures. Application of common methods for noise reduction like delay filtering and remote reference processing, only worked well for periods <1 s. Within the framework of this thesis two new filtering approaches were developed to handle the severe noise in long period data and obtain reliable processing results. The first algorithm is based on the Wiener filter in combination with a spike detection algorithm. Comparison of data variances of a local site with those of a reference site allows the identification of disturbed time series windows for each recorded channel at the local site. Using the data of the reference site, a Wiener filter algorithm is applied to predict physically meaningful data to replace the disturbed windows. While spikes in the magnetic channels are easily recognized and replaced, steps in the electric channels are more difficult to detect depending on their offset. Therefore, I have implemented a novel approach based on time series differentiation, noise removal and subsequent integration to overcome this obstacle. A second filtering approach where spikes and steps in the time series are identified using a comparison of the short and long time average of the data was also implemented as part of my thesis. For this filtering approach the noise in the form of spikes and offsets in the data is treated by an interpolation of the affected data samples. The new developments resulted in a substantial data improvement and allowed to gain one to two decades of data (up to 10 or 100 s). The re-processed MT data were used to image the electrical conductivity distribution of the BGB by 2D and 3D inversion. Inversion models are in good agreement with the surface geology delineating the highly resistive rocks of the BGB from surrounding more conductive geological units. Fault zones appear as conductive structures and can be traced to depths of 5 to 10 km. 2D models suggest a continuation of the faults further south across the boundary of the BGB. Based on the shallow tectonic structures (fault system) within the BGB compared to deeply rooted resistive batholiths in the area, tectonic models including both vertical mass transport and in parts present-day style plate tectonics seem to be most likely for the evolution of the BGB.</subfield></datafield><datafield tag="655" ind1=" " ind2="7"><subfield code="a">Hochschulschrift</subfield><subfield code="0">(DE-588)4113937-9</subfield><subfield code="0">(DE-627)105825778</subfield><subfield code="0">(DE-576)209480580</subfield><subfield code="2">gnd-content</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="D">g</subfield><subfield code="0">(DE-588)4589361-5</subfield><subfield code="0">(DE-627)325955743</subfield><subfield code="0">(DE-576)214014967</subfield><subfield code="a">Barberton Greenstone Belt</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="D">s</subfield><subfield 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