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Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 188-196

XIE Yuan, WANG Jian, LIU JiaDuo, LUO JianNing, ZHANG ShaoNan, YANG BaoNing, LI MingHui. Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 188-196.
Citation: XIE Yuan, WANG Jian, LIU JiaDuo, LUO JianNing, ZHANG ShaoNan, YANG BaoNing, LI MingHui. Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 188-196.
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Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin

  • 1.

    Chengdu instit ute of geology and mineral resources, Chengdu 610082;

  • 2.

    Chengdu university of technology, Chengdu 610059

  • Received Date: 2001-12-24
  • Publish Date: 2002-04-10
  • A series of steady carbonate and clastic rocks of coastal-shallow sea facies were deposited in the Nadigangri area,Qiangtang Basin,during the middle Jurassic. The middle Jurassic can be divided into five 3rd-graded sequences through sequence interpretation . On the basis of C, O and Sr isotopic compositions of four of those, δ13 C、δ180、N(87Sr/86Sr) values are all of distinct difference and regularity among different sequences, sequence boundaries and systems stracts. It is suggested that the going up and down of sea level occurred many times and the climate and tectonics change during the middle Jurassic, which controlled the formation and evolution of the middle Jurassic sequences. As a result, C, O and Sr isotopes can provide some quantitative geological and geochemical evidence for analyzing the middle Jurassic sequence.
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  • Received:  2001-12-24
  • Published:  2002-04-10

Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin

  • 1. Chengdu instit ute of geology and mineral resources, Chengdu 610082;
  • 2. Chengdu university of technology, Chengdu 610059
  • Received Date: 2001-12-24
  • Publish Date: 2002-04-10

Abstract: A series of steady carbonate and clastic rocks of coastal-shallow sea facies were deposited in the Nadigangri area,Qiangtang Basin,during the middle Jurassic. The middle Jurassic can be divided into five 3rd-graded sequences through sequence interpretation . On the basis of C, O and Sr isotopic compositions of four of those, δ13 C、δ180、N(87Sr/86Sr) values are all of distinct difference and regularity among different sequences, sequence boundaries and systems stracts. It is suggested that the going up and down of sea level occurred many times and the climate and tectonics change during the middle Jurassic, which controlled the formation and evolution of the middle Jurassic sequences. As a result, C, O and Sr isotopes can provide some quantitative geological and geochemical evidence for analyzing the middle Jurassic sequence.

XIE Yuan, WANG Jian, LIU JiaDuo, LUO JianNing, ZHANG ShaoNan, YANG BaoNing, LI MingHui. Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 188-196.
Citation: XIE Yuan, WANG Jian, LIU JiaDuo, LUO JianNing, ZHANG ShaoNan, YANG BaoNing, LI MingHui. Carbon,Oxygen and Strontium Isotopic Responses of Carbonate Rocks and the Middle Jurassic Squence Stratigraphy in the Nadigangri Area,Qiangtang Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 188-196.
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