Two stages of skarn formation - two tin enrichments : Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany

Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the se...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Lefebvre, Marie G. [verfasserIn] Romer, Rolf L. [akademischer betreuerIn] Melcher, Frank [akademischer betreuerIn] Altenberger, Uwe [verfasserIn]
Körperschaften:	Universität Potsdam [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Universität Potsdam ; 2019

Format:	E-Book
Sprache:	Englisch

Erschienen:	Potsdam: 2019

Schlagwörter:	Pöhla / Eibenstock / Skarn / Erzlagerstätte / Lagerstättenkunde Erzgebirge / Zinnstein / Polymetallische Lagerstätte / Geochemie / Greisen / Lagerstättenbildung Pöhla / Zinnlagerstätte / Wolframlagerstätte / Mineralisation / Metallogenese / Zinnerz
Formangabe:	Hochschulschrift

Anmerkung:	Kumulative Dissertation
Umfang:	1 Online-Ressource (VII, 87 Seiten, 7229 KB) ; Illustrationen, Diagramme

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Lefebvre, Marie G.: Two stages of skarn formation - two tin enrichments - Potsdam, 2019

Links:	Link aufrufen Volltext Volltext Link aufrufen Link aufrufen Link aufrufen

DOI / URN:	urn:nbn:de:kobv:517-opus4-427178 10.25932/publishup-42717

Katalog-ID:	1665704144

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245	1	0	\|a Two stages of skarn formation - two tin enrichments \|b Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany \|c von Marie G. Lefebvre
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520			\|a Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ...
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topic_title	553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd
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title_full	Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre
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title_sub	Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany
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title_sort	two stages of skarn formation - two tin enrichmentshämmerlein polymetallic skarn deposit, western erzgebirge, germany
title_auth	Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany
abstract	Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Kumulative Dissertation
abstractGer	Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Kumulative Dissertation
abstract_unstemmed	Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Kumulative Dissertation
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author2	Romer, Rolf L. Melcher, Frank Altenberger, Uwe Universität Potsdam
author2Str	Romer, Rolf L. Melcher, Frank Altenberger, Uwe Universität Potsdam
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hochschulschrift_bool	true
author2_role	dgs dgs
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hierarchy_sort_str	2019
bklnumber	38.52 38.55
allfields	1218496142 DE-101 urn:nbn:de:kobv:517-opus4-427178 urn 10.25932/publishup-42717 doi (DE-627)1665704144 (DE-599)KXP1665704144 (OCoLC)1197935620 DE-627 ger DE-627 rda eng XA-DE 553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Lefebvre, Marie G. verfasserin (DE-588)1186281162 (DE-627)1665795832 aut Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre Übersetzung des Haupttitels Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung Potsdam 2019 1 Online-Ressource (VII, 87 Seiten, 7229 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Dissertation Universität Potsdam 2019 Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd (DE-627) g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd (DE-627) Romer, Rolf L. akademischer betreuerin dgs Melcher, Frank akademischer betreuerin (DE-588)1166992802 (DE-627)1030841756 (DE-576)510988423 dgs Altenberger, Uwe verfasserin (DE-588)171949099 (DE-627)696840650 (DE-576)132826798 aut Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Erscheint auch als Druck-Ausgabe Lefebvre, Marie G. Two stages of skarn formation - two tin enrichments Potsdam, 2019 VII, 87 Seiten (DE-627)1665704705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-42717 Resolving-System kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-427178 2020-10-07 Resolving-System https://d-nb.info/1218496142/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/42717 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO 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_2403 ISIL_DE-LFER 38.52 Geologie der Erze SEPA (DE-627)106404865 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 553 20 01 0084 3782408020 x 20-10-20 21 01 0046 3782447247 z 20-10-20 22 01 0018 3782486498 SUBolrd xu 20-10-20 23 01 0830 3782524705 olr-d x 20-10-20 30 01 0104 3782548116 z 20-10-20 40 01 0007 3782570294 xsn 20-10-20 60 01 0705 3782608569 OLRD z 20-10-20 63 01 3401 3782645839 ORD x 20-10-20 65 01 0003 4168407632 GBV-ODiss Open Access z 17-07-22 70 01 0089 3782666070 zdo 20-10-20 105 01 0841 3782873211 z 20-10-20 110 01 3110 3782690443 x 20-10-20 132 01 0959 3782716256 OLR-DISS x 20-10-20 151 01 0546 3782753097 OLR-ODISS z 20-10-20 161 01 0960 3782768795 ORD z 20-10-20 285 01 0517 3475990040 z 15-05-19 293 01 3293 3782844335 ORD z 20-10-20 370 01 4370 3782866606 x 20-10-20 2403 01 DE-LFER 3480689728 00 --%%-- --%%-- n --%%-- l01 02-06-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 285 01 0517 https://doi.org/10.25932/publishup-42717 LF 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 2403 01 DE-LFER https://doi.org/10.25932/publishup-42717 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TH 5050 285 00 DE-517 00 TP 5231 20 01 0084 OLRD 110 01 3110 OLRD 285 01 0517 $f9300$ds 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
spelling	1218496142 DE-101 urn:nbn:de:kobv:517-opus4-427178 urn 10.25932/publishup-42717 doi (DE-627)1665704144 (DE-599)KXP1665704144 (OCoLC)1197935620 DE-627 ger DE-627 rda eng XA-DE 553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Lefebvre, Marie G. verfasserin (DE-588)1186281162 (DE-627)1665795832 aut Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre Übersetzung des Haupttitels Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung Potsdam 2019 1 Online-Ressource (VII, 87 Seiten, 7229 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Dissertation Universität Potsdam 2019 Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd (DE-627) g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd (DE-627) Romer, Rolf L. akademischer betreuerin dgs Melcher, Frank akademischer betreuerin (DE-588)1166992802 (DE-627)1030841756 (DE-576)510988423 dgs Altenberger, Uwe verfasserin (DE-588)171949099 (DE-627)696840650 (DE-576)132826798 aut Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Erscheint auch als Druck-Ausgabe Lefebvre, Marie G. Two stages of skarn formation - two tin enrichments Potsdam, 2019 VII, 87 Seiten (DE-627)1665704705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-42717 Resolving-System kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-427178 2020-10-07 Resolving-System https://d-nb.info/1218496142/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/42717 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO 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_2403 ISIL_DE-LFER 38.52 Geologie der Erze SEPA (DE-627)106404865 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 553 20 01 0084 3782408020 x 20-10-20 21 01 0046 3782447247 z 20-10-20 22 01 0018 3782486498 SUBolrd xu 20-10-20 23 01 0830 3782524705 olr-d x 20-10-20 30 01 0104 3782548116 z 20-10-20 40 01 0007 3782570294 xsn 20-10-20 60 01 0705 3782608569 OLRD z 20-10-20 63 01 3401 3782645839 ORD x 20-10-20 65 01 0003 4168407632 GBV-ODiss Open Access z 17-07-22 70 01 0089 3782666070 zdo 20-10-20 105 01 0841 3782873211 z 20-10-20 110 01 3110 3782690443 x 20-10-20 132 01 0959 3782716256 OLR-DISS x 20-10-20 151 01 0546 3782753097 OLR-ODISS z 20-10-20 161 01 0960 3782768795 ORD z 20-10-20 285 01 0517 3475990040 z 15-05-19 293 01 3293 3782844335 ORD z 20-10-20 370 01 4370 3782866606 x 20-10-20 2403 01 DE-LFER 3480689728 00 --%%-- --%%-- n --%%-- l01 02-06-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 285 01 0517 https://doi.org/10.25932/publishup-42717 LF 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 2403 01 DE-LFER https://doi.org/10.25932/publishup-42717 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TH 5050 285 00 DE-517 00 TP 5231 20 01 0084 OLRD 110 01 3110 OLRD 285 01 0517 $f9300$ds 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	1218496142 DE-101 urn:nbn:de:kobv:517-opus4-427178 urn 10.25932/publishup-42717 doi (DE-627)1665704144 (DE-599)KXP1665704144 (OCoLC)1197935620 DE-627 ger DE-627 rda eng XA-DE 553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Lefebvre, Marie G. verfasserin (DE-588)1186281162 (DE-627)1665795832 aut Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre Übersetzung des Haupttitels Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung Potsdam 2019 1 Online-Ressource (VII, 87 Seiten, 7229 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Dissertation Universität Potsdam 2019 Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd (DE-627) g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd (DE-627) Romer, Rolf L. akademischer betreuerin dgs Melcher, Frank akademischer betreuerin (DE-588)1166992802 (DE-627)1030841756 (DE-576)510988423 dgs Altenberger, Uwe verfasserin (DE-588)171949099 (DE-627)696840650 (DE-576)132826798 aut Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Erscheint auch als Druck-Ausgabe Lefebvre, Marie G. Two stages of skarn formation - two tin enrichments Potsdam, 2019 VII, 87 Seiten (DE-627)1665704705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-42717 Resolving-System kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-427178 2020-10-07 Resolving-System https://d-nb.info/1218496142/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/42717 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO 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_2403 ISIL_DE-LFER 38.52 Geologie der Erze SEPA (DE-627)106404865 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 553 20 01 0084 3782408020 x 20-10-20 21 01 0046 3782447247 z 20-10-20 22 01 0018 3782486498 SUBolrd xu 20-10-20 23 01 0830 3782524705 olr-d x 20-10-20 30 01 0104 3782548116 z 20-10-20 40 01 0007 3782570294 xsn 20-10-20 60 01 0705 3782608569 OLRD z 20-10-20 63 01 3401 3782645839 ORD x 20-10-20 65 01 0003 4168407632 GBV-ODiss Open Access z 17-07-22 70 01 0089 3782666070 zdo 20-10-20 105 01 0841 3782873211 z 20-10-20 110 01 3110 3782690443 x 20-10-20 132 01 0959 3782716256 OLR-DISS x 20-10-20 151 01 0546 3782753097 OLR-ODISS z 20-10-20 161 01 0960 3782768795 ORD z 20-10-20 285 01 0517 3475990040 z 15-05-19 293 01 3293 3782844335 ORD z 20-10-20 370 01 4370 3782866606 x 20-10-20 2403 01 DE-LFER 3480689728 00 --%%-- --%%-- n --%%-- l01 02-06-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 285 01 0517 https://doi.org/10.25932/publishup-42717 LF 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 2403 01 DE-LFER https://doi.org/10.25932/publishup-42717 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TH 5050 285 00 DE-517 00 TP 5231 20 01 0084 OLRD 110 01 3110 OLRD 285 01 0517 $f9300$ds 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	1218496142 DE-101 urn:nbn:de:kobv:517-opus4-427178 urn 10.25932/publishup-42717 doi (DE-627)1665704144 (DE-599)KXP1665704144 (OCoLC)1197935620 DE-627 ger DE-627 rda eng XA-DE 553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Lefebvre, Marie G. verfasserin (DE-588)1186281162 (DE-627)1665795832 aut Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre Übersetzung des Haupttitels Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung Potsdam 2019 1 Online-Ressource (VII, 87 Seiten, 7229 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Dissertation Universität Potsdam 2019 Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd (DE-627) g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd (DE-627) Romer, Rolf L. akademischer betreuerin dgs Melcher, Frank akademischer betreuerin (DE-588)1166992802 (DE-627)1030841756 (DE-576)510988423 dgs Altenberger, Uwe verfasserin (DE-588)171949099 (DE-627)696840650 (DE-576)132826798 aut Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Erscheint auch als Druck-Ausgabe Lefebvre, Marie G. Two stages of skarn formation - two tin enrichments Potsdam, 2019 VII, 87 Seiten (DE-627)1665704705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-42717 Resolving-System kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-427178 2020-10-07 Resolving-System https://d-nb.info/1218496142/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/42717 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO 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_2403 ISIL_DE-LFER 38.52 Geologie der Erze SEPA (DE-627)106404865 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 553 20 01 0084 3782408020 x 20-10-20 21 01 0046 3782447247 z 20-10-20 22 01 0018 3782486498 SUBolrd xu 20-10-20 23 01 0830 3782524705 olr-d x 20-10-20 30 01 0104 3782548116 z 20-10-20 40 01 0007 3782570294 xsn 20-10-20 60 01 0705 3782608569 OLRD z 20-10-20 63 01 3401 3782645839 ORD x 20-10-20 65 01 0003 4168407632 GBV-ODiss Open Access z 17-07-22 70 01 0089 3782666070 zdo 20-10-20 105 01 0841 3782873211 z 20-10-20 110 01 3110 3782690443 x 20-10-20 132 01 0959 3782716256 OLR-DISS x 20-10-20 151 01 0546 3782753097 OLR-ODISS z 20-10-20 161 01 0960 3782768795 ORD z 20-10-20 285 01 0517 3475990040 z 15-05-19 293 01 3293 3782844335 ORD z 20-10-20 370 01 4370 3782866606 x 20-10-20 2403 01 DE-LFER 3480689728 00 --%%-- --%%-- n --%%-- l01 02-06-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 285 01 0517 https://doi.org/10.25932/publishup-42717 LF 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 2403 01 DE-LFER https://doi.org/10.25932/publishup-42717 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TH 5050 285 00 DE-517 00 TP 5231 20 01 0084 OLRD 110 01 3110 OLRD 285 01 0517 $f9300$ds 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
allfieldsSound	1218496142 DE-101 urn:nbn:de:kobv:517-opus4-427178 urn 10.25932/publishup-42717 doi (DE-627)1665704144 (DE-599)KXP1665704144 (OCoLC)1197935620 DE-627 ger DE-627 rda eng XA-DE 553 DE-101 550 DE-101 38.52 bkl 38.55 bkl Lefebvre, Marie G. verfasserin (DE-588)1186281162 (DE-627)1665795832 aut Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany von Marie G. Lefebvre Übersetzung des Haupttitels Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung Potsdam 2019 1 Online-Ressource (VII, 87 Seiten, 7229 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Dissertation Universität Potsdam 2019 Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. Tin was mobilized during both events. ... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd g (DE-588)4577623-4 (DE-627)325130477 (DE-576)213893290 Eibenstock Region gnd s (DE-588)4290972-7 (DE-627)104237023 (DE-576)210837799 Skarn gnd s (DE-588)4015501-8 (DE-627)104222263 (DE-576)208911979 Erzlagerstätte gnd s (DE-588)4140085-9 (DE-627)105630470 (DE-576)209699825 Lagerstättenkunde gnd (DE-627) g (DE-588)4091909-2 (DE-627)104742402 (DE-576)209285419 Erzgebirge West gnd s (DE-588)4067842-8 (DE-627)106107321 (DE-576)209171731 Zinnstein gnd s (DE-588)4426603-0 (DE-627)216503159 (DE-576)212327232 Polymetallische Lagerstätte gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4356668-6 (DE-627)18127793X (DE-576)211583731 Greisen gnd s (DE-588)4166450-4 (DE-627)105432598 (DE-576)209902027 Lagerstättenbildung gnd (DE-627) g (DE-588)4746440-9 (DE-627)371027713 (DE-576)215962192 Pöhla gnd s (DE-588)4213747-0 (DE-627)105070505 (DE-576)210216417 Zinnlagerstätte gnd s (DE-588)4196785-9 (DE-627)105201359 (DE-576)210110112 Wolframlagerstätte gnd s (DE-588)4132279-4 (DE-627)105688932 (DE-576)209634227 Mineralisation gnd s (DE-588)4122281-7 (DE-627)105763608 (DE-576)209550104 Metallogenese gnd s (DE-588)4190892-2 (DE-627)105246263 (DE-576)210069848 Zinnerz gnd (DE-627) Romer, Rolf L. akademischer betreuerin dgs Melcher, Frank akademischer betreuerin (DE-588)1166992802 (DE-627)1030841756 (DE-576)510988423 dgs Altenberger, Uwe verfasserin (DE-588)171949099 (DE-627)696840650 (DE-576)132826798 aut Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Erscheint auch als Druck-Ausgabe Lefebvre, Marie G. Two stages of skarn formation - two tin enrichments Potsdam, 2019 VII, 87 Seiten (DE-627)1665704705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 Resolving-System kostenfrei Volltext https://doi.org/10.25932/publishup-42717 Resolving-System kostenfrei Volltext https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-427178 2020-10-07 Resolving-System https://d-nb.info/1218496142/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/42717 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO 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_2403 ISIL_DE-LFER 38.52 Geologie der Erze SEPA (DE-627)106404865 38.55 Regionale Geologie SEPA (DE-627)106407260 BO 045F 553 20 01 0084 3782408020 x 20-10-20 21 01 0046 3782447247 z 20-10-20 22 01 0018 3782486498 SUBolrd xu 20-10-20 23 01 0830 3782524705 olr-d x 20-10-20 30 01 0104 3782548116 z 20-10-20 40 01 0007 3782570294 xsn 20-10-20 60 01 0705 3782608569 OLRD z 20-10-20 63 01 3401 3782645839 ORD x 20-10-20 65 01 0003 4168407632 GBV-ODiss Open Access z 17-07-22 70 01 0089 3782666070 zdo 20-10-20 105 01 0841 3782873211 z 20-10-20 110 01 3110 3782690443 x 20-10-20 132 01 0959 3782716256 OLR-DISS x 20-10-20 151 01 0546 3782753097 OLR-ODISS z 20-10-20 161 01 0960 3782768795 ORD z 20-10-20 285 01 0517 3475990040 z 15-05-19 293 01 3293 3782844335 ORD z 20-10-20 370 01 4370 3782866606 x 20-10-20 2403 01 DE-LFER 3480689728 00 --%%-- --%%-- n --%%-- l01 02-06-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 40 01 0007 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 285 01 0517 https://doi.org/10.25932/publishup-42717 LF 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427178 2403 01 DE-LFER https://doi.org/10.25932/publishup-42717 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TH 5050 285 00 DE-517 00 TP 5231 20 01 0084 OLRD 110 01 3110 OLRD 285 01 0517 $f9300$ds 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
language	English
format_phy_str_mv	Book
bklname	Geologie der Erze Regionale Geologie
institution	findex.gbv.de
selectbib_iln_str_mv	20@ 21@ 22@u 23@ 30@ 40@sn 60@ 63@ 65@ 70@do 105@ 110@ 132@ 151@ 161@ 285@ 293@ 370@ 2403@01
dewey-raw	553
authorswithroles_txt_mv	Lefebvre, Marie G. @@aut@@ Romer, Rolf L. @@dgs@@ Melcher, Frank @@dgs@@ Altenberger, Uwe @@aut@@
genre_facet	Hochschulschrift
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Lefebvre</subfield></datafield><datafield tag="246" ind1="1" ind2=" "><subfield code="i">Übersetzung des Haupttitels</subfield><subfield code="a">Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Potsdam</subfield><subfield code="c">2019</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (VII, 87 Seiten, 7229 KB)</subfield><subfield code="b">Illustrationen, Diagramme</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="500" ind1=" " ind2=" "><subfield code="a">Kumulative Dissertation</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Universität Potsdam</subfield><subfield code="d">2019</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Skarn deposits are found on every continents and were formed at different times from Precambrian to Tertiary. Typically, the formation of a skarn is induced by a granitic intrusion in carbonates-rich sedimentary rocks. During contact metamorphism, fluids derived from the granite interact with the sedimentary host rocks, which results in the formation of calc-silicate minerals at the expense of carbonates. Those newly formed minerals generally develop in a metamorphic zoned aureole with garnet in the proximal and pyroxene in the distal zone. Ore elements contained in magmatic fluids are precipitated due to the change in fluid composition. The temperature decrease of the entire system, due to the cooling of magmatic fluids and the entering of meteoric water, allows retrogression of some prograde minerals. The Hämmerlein skarn deposit has a multi-stage history with a skarn formation during regional metamorphism and a retrogression of primary skarn minerals during the granitic intrusion. 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author	Lefebvre, Marie G.
spellingShingle	Lefebvre, Marie G. ddc 553 ddc 550 bkl 38.52 bkl 38.55 gnd Pöhla gnd Eibenstock gnd Skarn gnd Erzlagerstätte gnd Lagerstättenkunde gnd Erzgebirge gnd Zinnstein gnd Polymetallische Lagerstätte gnd Geochemie gnd Greisen gnd Lagerstättenbildung gnd Zinnlagerstätte gnd Wolframlagerstätte gnd Mineralisation gnd Metallogenese gnd Zinnerz Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany
authorStr	Lefebvre, Marie G.
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topic	ddc 553 ddc 550 bkl 38.52 bkl 38.55 gnd Pöhla gnd Eibenstock gnd Skarn gnd Erzlagerstätte gnd Lagerstättenkunde gnd Erzgebirge gnd Zinnstein gnd Polymetallische Lagerstätte gnd Geochemie gnd Greisen gnd Lagerstättenbildung gnd Zinnlagerstätte gnd Wolframlagerstätte gnd Mineralisation gnd Metallogenese gnd Zinnerz
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dewey-tens	550 - Earth sciences & geology
title	Two stages of skarn formation - two tin enrichments Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany
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author_browse	Lefebvre, Marie G. Altenberger, Uwe
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title_short	Two stages of skarn formation - two tin enrichments
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GND_txt_mv	Lefebvre, Marie Lefebvre, M. G. Lefebvre, M. Lefebvre, Marie G. Hochschulschrift Gemeinde Pöhla Pöhla Eibenstock (Region) Skarn Erz / Lagerstätte Erzlagerstätte Rohstoffgeologie <Quasisynonym> Lagerstättenlehre Lagerstättengeologie Lagerstättenkunde Westerzgebirge Westliches Erzgebirge Erzgebirge (West) Kassiterit Cassiterit Zinnstein Polymetallische Lagerstätte Lithogeochemie Gesteinschemie Geochemie Greisen Lagerstättenbildung Zinnerzlagerstätte Zinn / Erzlagerstätte Zinn / Lagerstätte Zinnerz / Erzlagerstätte Zinnlagerstätte Wolfram / Lagerstätte Wolframlagerstätte Mineralisierung Mineralisation Erzlagerstättenbildung Metallogenese Zinn / Erz Zinnerz Melcher, F. Melcher, Frank Altenberger, U. Altenburger, Uwe Altenberger, Uwe Uni Potsdam Potsdamer Universität Univ. Potsdam University of Potsdam Universität Potsdam
GND_txtF_mv	Lefebvre, Marie Lefebvre, M. G. Lefebvre, M. Lefebvre, Marie G. Hochschulschrift Gemeinde Pöhla Pöhla Eibenstock (Region) Skarn Erz / Lagerstätte Erzlagerstätte Rohstoffgeologie <Quasisynonym> Lagerstättenlehre Lagerstättengeologie Lagerstättenkunde Westerzgebirge Westliches Erzgebirge Erzgebirge (West) Kassiterit Cassiterit Zinnstein Polymetallische Lagerstätte Lithogeochemie Gesteinschemie Geochemie Greisen Lagerstättenbildung Zinnerzlagerstätte Zinn / Erzlagerstätte Zinn / Lagerstätte Zinnerz / Erzlagerstätte Zinnlagerstätte Wolfram / Lagerstätte Wolframlagerstätte Mineralisierung Mineralisation Erzlagerstättenbildung Metallogenese Zinn / Erz Zinnerz Melcher, F. Melcher, Frank Altenberger, U. Altenburger, Uwe Altenberger, Uwe Uni Potsdam Potsdamer Universität Univ. Potsdam University of Potsdam Universität Potsdam
title_alt	Zwei Stufen der Skarn-Bildung - zwei Phasen der Zinnmobilisierung
doi_str	10.25932/publishup-42717
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up_date	2024-07-05T02:14:46.419Z
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Two stages of skarn formation - two tin enrichments : Hämmerlein polymetallic skarn deposit, western Erzgebirge, Germany

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