Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation
Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Fürsich, Franz T. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2003 |
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| Schlagwörter: |
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| Anmerkung: |
© Institut für Palaentologie, Universitat Erlangen 2003 |
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| Übergeordnetes Werk: |
Enthalten in: Facies - Springer-Verlag, 1979, 48(2003), 1 vom: Dez., Seite 151-170 |
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| Übergeordnetes Werk: |
volume:48 ; year:2003 ; number:1 ; month:12 ; pages:151-170 |
| Links: |
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| DOI / URN: |
10.1007/BF02667537 |
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| Katalog-ID: |
OLC2075395128 |
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| 245 | 1 | 0 | |a Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation |
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| 520 | |a Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. | ||
| 650 | 4 | |a Synsedimentary Tectonics | |
| 650 | 4 | |a Stratigraphy | |
| 650 | 4 | |a Iran | |
| 650 | 4 | |a Jurassic (Callovian) | |
| 700 | 1 | |a Wilmsen, Markus |4 aut | |
| 700 | 1 | |a Seyed-Emami, Kazem |4 aut | |
| 700 | 1 | |a Majidifard, Mahmoud R. |4 aut | |
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10.1007/BF02667537 doi (DE-627)OLC2075395128 (DE-He213)BF02667537-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Fürsich, Franz T. verfasserin aut Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Palaentologie, Universitat Erlangen 2003 Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) Wilmsen, Markus aut Seyed-Emami, Kazem aut Majidifard, Mahmoud R. aut Enthalten in Facies Springer-Verlag, 1979 48(2003), 1 vom: Dez., Seite 151-170 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:48 year:2003 number:1 month:12 pages:151-170 https://doi.org/10.1007/BF02667537 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_154 GBV_ILN_188 GBV_ILN_267 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4307 AR 48 2003 1 12 151-170 |
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10.1007/BF02667537 doi (DE-627)OLC2075395128 (DE-He213)BF02667537-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Fürsich, Franz T. verfasserin aut Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Palaentologie, Universitat Erlangen 2003 Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) Wilmsen, Markus aut Seyed-Emami, Kazem aut Majidifard, Mahmoud R. aut Enthalten in Facies Springer-Verlag, 1979 48(2003), 1 vom: Dez., Seite 151-170 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:48 year:2003 number:1 month:12 pages:151-170 https://doi.org/10.1007/BF02667537 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_154 GBV_ILN_188 GBV_ILN_267 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4307 AR 48 2003 1 12 151-170 |
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10.1007/BF02667537 doi (DE-627)OLC2075395128 (DE-He213)BF02667537-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Fürsich, Franz T. verfasserin aut Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Palaentologie, Universitat Erlangen 2003 Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) Wilmsen, Markus aut Seyed-Emami, Kazem aut Majidifard, Mahmoud R. aut Enthalten in Facies Springer-Verlag, 1979 48(2003), 1 vom: Dez., Seite 151-170 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:48 year:2003 number:1 month:12 pages:151-170 https://doi.org/10.1007/BF02667537 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_154 GBV_ILN_188 GBV_ILN_267 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4307 AR 48 2003 1 12 151-170 |
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10.1007/BF02667537 doi (DE-627)OLC2075395128 (DE-He213)BF02667537-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Fürsich, Franz T. verfasserin aut Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Palaentologie, Universitat Erlangen 2003 Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) Wilmsen, Markus aut Seyed-Emami, Kazem aut Majidifard, Mahmoud R. aut Enthalten in Facies Springer-Verlag, 1979 48(2003), 1 vom: Dez., Seite 151-170 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:48 year:2003 number:1 month:12 pages:151-170 https://doi.org/10.1007/BF02667537 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_154 GBV_ILN_188 GBV_ILN_267 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4307 AR 48 2003 1 12 151-170 |
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10.1007/BF02667537 doi (DE-627)OLC2075395128 (DE-He213)BF02667537-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Fürsich, Franz T. verfasserin aut Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Palaentologie, Universitat Erlangen 2003 Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) Wilmsen, Markus aut Seyed-Emami, Kazem aut Majidifard, Mahmoud R. aut Enthalten in Facies Springer-Verlag, 1979 48(2003), 1 vom: Dez., Seite 151-170 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:48 year:2003 number:1 month:12 pages:151-170 https://doi.org/10.1007/BF02667537 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_154 GBV_ILN_188 GBV_ILN_267 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4307 AR 48 2003 1 12 151-170 |
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Enthalten in Facies 48(2003), 1 vom: Dez., Seite 151-170 volume:48 year:2003 number:1 month:12 pages:151-170 |
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All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. 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Fürsich, Franz T. ddc 550 ssgn 13 misc Synsedimentary Tectonics misc Stratigraphy misc Iran misc Jurassic (Callovian) Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation |
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550 VZ 13 ssgn Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation Synsedimentary Tectonics Stratigraphy Iran Jurassic (Callovian) |
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Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation |
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Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation |
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evidence of synsedimentary tectonics in the northern tabas block, east-central iran: the callovian (middle jurassic) sikhor formation |
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Evidence of synsedimentary tectonics in the Northern Tabas Block, East-Central Iran: The Callovian (Middle Jurassic) Sikhor Formation |
| abstract |
Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. © Institut für Palaentologie, Universitat Erlangen 2003 |
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Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. © Institut für Palaentologie, Universitat Erlangen 2003 |
| abstract_unstemmed |
Summary The Sikhor Formation (new) is a predominantly siliciclastic sediment package intercalated between the marly-silty Baghamshah Formation (below) and the calcareous Esfandiar Limestone and Qal'eh Dokhtar Limestone formations (above). All stratigraphic evidence points to an Early Callovian age of the formation. The Sikhor Formation is restricted to the southern and central Shotori Mountains and consists of two members: The Kuh-e-Neygu Member (new) is composed of fluvialdeltaic conglomerates, sandstones, and siltstones grading into marly silt of the Baghamshah Formation. The overlying Majd Member (new) is characterised by mixed siliciclastic-carbonate sediments that record the interfingering of carbonate ramp sediments with fluvialdeltaic sands and silts. Evidence of erosional truncation of the underlying Baghamshah Formation and confinement of the siliciclastic sediment to a comparatively narrow, NNW-SSE elongated strip suggest that the formation had its origin in the asymmetric uplift of a westdipping tilted fault block in the southern Shotori Mountains that shed its sediment predominantly in a northern and eastern direction. After erosional levelling, the former uplifted areas were overgrown by the highly productive Esfandiar Carbonate Platform. The Sikhor Formation thus is evidence of an extensional tectonic pulse in the early Callovian and underlines that this area of the Tabas Block was a tectonically highly unstable area during most of the Jurassic. © Institut für Palaentologie, Universitat Erlangen 2003 |
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