Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan
Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spann...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gaetani, Maurizio [verfasserIn] Nicora, Alda [verfasserIn] Henderson, Charles [verfasserIn] Cirilli, Simonetta [verfasserIn] Gale, Luka [verfasserIn] Rettori, Roberto [verfasserIn] Vuolo, Irene [verfasserIn] Atudorei, Viorel [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Facies - Berlin : Springer, 1979, 59(2012), 4 vom: 05. Dez., Seite 915-948 |
|---|---|
| Übergeordnetes Werk: |
volume:59 ; year:2012 ; number:4 ; day:05 ; month:12 ; pages:915-948 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10347-012-0346-9 |
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| Katalog-ID: |
SPR009788271 |
|---|
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| 245 | 1 | 0 | |a Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
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| 520 | |a Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. | ||
| 650 | 4 | |a Permian |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Triassic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Jurassic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Karakorum |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Pakistan |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Conodonts |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Foraminifers |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Palynostratigraphy |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Carbon isotopes |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Nicora, Alda |e verfasserin |4 aut | |
| 700 | 1 | |a Henderson, Charles |e verfasserin |4 aut | |
| 700 | 1 | |a Cirilli, Simonetta |e verfasserin |4 aut | |
| 700 | 1 | |a Gale, Luka |e verfasserin |4 aut | |
| 700 | 1 | |a Rettori, Roberto |e verfasserin |4 aut | |
| 700 | 1 | |a Vuolo, Irene |e verfasserin |4 aut | |
| 700 | 1 | |a Atudorei, Viorel |e verfasserin |4 aut | |
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10.1007/s10347-012-0346-9 doi (DE-627)SPR009788271 (SPR)s10347-012-0346-9-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE 38.20 bkl 38.16 bkl Gaetani, Maurizio verfasserin aut Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 Nicora, Alda verfasserin aut Henderson, Charles verfasserin aut Cirilli, Simonetta verfasserin aut Gale, Luka verfasserin aut Rettori, Roberto verfasserin aut Vuolo, Irene verfasserin aut Atudorei, Viorel verfasserin aut Enthalten in Facies Berlin : Springer, 1979 59(2012), 4 vom: 05. Dez., Seite 915-948 (DE-627)328204684 (DE-600)2045898-8 1612-4820 nnns volume:59 year:2012 number:4 day:05 month:12 pages:915-948 https://dx.doi.org/10.1007/s10347-012-0346-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.20 ASE 38.16 ASE AR 59 2012 4 05 12 915-948 |
| spelling |
10.1007/s10347-012-0346-9 doi (DE-627)SPR009788271 (SPR)s10347-012-0346-9-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE 38.20 bkl 38.16 bkl Gaetani, Maurizio verfasserin aut Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 Nicora, Alda verfasserin aut Henderson, Charles verfasserin aut Cirilli, Simonetta verfasserin aut Gale, Luka verfasserin aut Rettori, Roberto verfasserin aut Vuolo, Irene verfasserin aut Atudorei, Viorel verfasserin aut Enthalten in Facies Berlin : Springer, 1979 59(2012), 4 vom: 05. Dez., Seite 915-948 (DE-627)328204684 (DE-600)2045898-8 1612-4820 nnns volume:59 year:2012 number:4 day:05 month:12 pages:915-948 https://dx.doi.org/10.1007/s10347-012-0346-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.20 ASE 38.16 ASE AR 59 2012 4 05 12 915-948 |
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10.1007/s10347-012-0346-9 doi (DE-627)SPR009788271 (SPR)s10347-012-0346-9-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE 38.20 bkl 38.16 bkl Gaetani, Maurizio verfasserin aut Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 Nicora, Alda verfasserin aut Henderson, Charles verfasserin aut Cirilli, Simonetta verfasserin aut Gale, Luka verfasserin aut Rettori, Roberto verfasserin aut Vuolo, Irene verfasserin aut Atudorei, Viorel verfasserin aut Enthalten in Facies Berlin : Springer, 1979 59(2012), 4 vom: 05. Dez., Seite 915-948 (DE-627)328204684 (DE-600)2045898-8 1612-4820 nnns volume:59 year:2012 number:4 day:05 month:12 pages:915-948 https://dx.doi.org/10.1007/s10347-012-0346-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.20 ASE 38.16 ASE AR 59 2012 4 05 12 915-948 |
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10.1007/s10347-012-0346-9 doi (DE-627)SPR009788271 (SPR)s10347-012-0346-9-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE 38.20 bkl 38.16 bkl Gaetani, Maurizio verfasserin aut Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 Nicora, Alda verfasserin aut Henderson, Charles verfasserin aut Cirilli, Simonetta verfasserin aut Gale, Luka verfasserin aut Rettori, Roberto verfasserin aut Vuolo, Irene verfasserin aut Atudorei, Viorel verfasserin aut Enthalten in Facies Berlin : Springer, 1979 59(2012), 4 vom: 05. Dez., Seite 915-948 (DE-627)328204684 (DE-600)2045898-8 1612-4820 nnns volume:59 year:2012 number:4 day:05 month:12 pages:915-948 https://dx.doi.org/10.1007/s10347-012-0346-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.20 ASE 38.16 ASE AR 59 2012 4 05 12 915-948 |
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10.1007/s10347-012-0346-9 doi (DE-627)SPR009788271 (SPR)s10347-012-0346-9-e DE-627 ger DE-627 rakwb eng 550 ASE 550 ASE 38.20 bkl 38.16 bkl Gaetani, Maurizio verfasserin aut Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 Nicora, Alda verfasserin aut Henderson, Charles verfasserin aut Cirilli, Simonetta verfasserin aut Gale, Luka verfasserin aut Rettori, Roberto verfasserin aut Vuolo, Irene verfasserin aut Atudorei, Viorel verfasserin aut Enthalten in Facies Berlin : Springer, 1979 59(2012), 4 vom: 05. Dez., Seite 915-948 (DE-627)328204684 (DE-600)2045898-8 1612-4820 nnns volume:59 year:2012 number:4 day:05 month:12 pages:915-948 https://dx.doi.org/10.1007/s10347-012-0346-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.20 ASE 38.16 ASE AR 59 2012 4 05 12 915-948 |
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Enthalten in Facies 59(2012), 4 vom: 05. Dez., Seite 915-948 volume:59 year:2012 number:4 day:05 month:12 pages:915-948 |
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Enthalten in Facies 59(2012), 4 vom: 05. Dez., Seite 915-948 volume:59 year:2012 number:4 day:05 month:12 pages:915-948 |
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Permian Triassic Jurassic Karakorum Pakistan Conodonts Foraminifers Palynostratigraphy Carbon isotopes |
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Gaetani, Maurizio @@aut@@ Nicora, Alda @@aut@@ Henderson, Charles @@aut@@ Cirilli, Simonetta @@aut@@ Gale, Luka @@aut@@ Rettori, Roberto @@aut@@ Vuolo, Irene @@aut@@ Atudorei, Viorel @@aut@@ |
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2012-12-05T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR009788271</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110213950.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2012 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10347-012-0346-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR009788271</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10347-012-0346-9-e</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">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.20</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.16</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Gaetani, Maurizio</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</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="520" ind1=" " ind2=" "><subfield code="a">Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. 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|
| author |
Gaetani, Maurizio |
| spellingShingle |
Gaetani, Maurizio ddc 550 bkl 38.20 bkl 38.16 misc Permian misc Triassic misc Jurassic misc Karakorum misc Pakistan misc Conodonts misc Foraminifers misc Palynostratigraphy misc Carbon isotopes Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
| authorStr |
Gaetani, Maurizio |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)328204684 |
| format |
electronic Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut aut aut |
| collection |
springer |
| remote_str |
true |
| illustrated |
Not Illustrated |
| issn |
1612-4820 |
| topic_title |
550 ASE 38.20 bkl 38.16 bkl Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan Permian (dpeaa)DE-He213 Triassic (dpeaa)DE-He213 Jurassic (dpeaa)DE-He213 Karakorum (dpeaa)DE-He213 Pakistan (dpeaa)DE-He213 Conodonts (dpeaa)DE-He213 Foraminifers (dpeaa)DE-He213 Palynostratigraphy (dpeaa)DE-He213 Carbon isotopes (dpeaa)DE-He213 |
| topic |
ddc 550 bkl 38.20 bkl 38.16 misc Permian misc Triassic misc Jurassic misc Karakorum misc Pakistan misc Conodonts misc Foraminifers misc Palynostratigraphy misc Carbon isotopes |
| topic_unstemmed |
ddc 550 bkl 38.20 bkl 38.16 misc Permian misc Triassic misc Jurassic misc Karakorum misc Pakistan misc Conodonts misc Foraminifers misc Palynostratigraphy misc Carbon isotopes |
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Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
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Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
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Gaetani, Maurizio |
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Gaetani, Maurizio Nicora, Alda Henderson, Charles Cirilli, Simonetta Gale, Luka Rettori, Roberto Vuolo, Irene Atudorei, Viorel |
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refinements in the upper permian to lower jurassic stratigraphy of karakorum, pakistan |
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Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
| abstract |
Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. |
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Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. |
| abstract_unstemmed |
Abstract New sampling on critical intervals of the uppermost Permian and Triassic successions of the Northern Karakorum Terrain in the Karakorum Range (Pakistan) has refined the stratigraphy. Two types of successions may be distinguished in the Karakorum Range: a carbonate platform succession, spanning the whole interval from Upper Permian to Upper Triassic, possibly with several gaps; and a basinal succession, deposited from the Middle Permian to Early Carnian (Late Triassic), when the carbonate platform prograded into the basin. With the approaching and later docking of the Karakorum Block against the Asian margin closing the Paleo-Tethys, a portion of Karakorum emerged while another part subsided as a fore-deep, receiving clastics from the emerging Cimmerian Range. Molassic sediments filled the basin, whilst shallow-water carbonates transgressed over the emerged carbonate platform sometime between the latest Triassic and the Pliensbachian (Early Jurassic), with Cimmerian deformation occurring to the north. The age control is provided by conodonts, with assemblages of late Wuchiapingian, Changhsingian, Induan (Griesbachian and Dienerian), late Olenekian, early Anisian, late Ladinian, and early Carnian ages, respectively. Some information on the section around the P/T boundary is provided by palynology and isotopic $ C^{13} $ values. The dating of the Norian/Rhaetian platform is provided by foraminifers. |
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Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan |
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| score |
7.4004154 |