The Origin of Paleokarst in the Huanglong Formation of the Eastern Sichuan Basin：Evidence from δ~（13）C, δ~（18）O and ~（87）Sr/~（86）Sr
Karst rocks from the Huanglong Formation exposed at the margin of the Eastern Sichuan Basin can be divided into four types：slightly corroded, moderately corroded porous, intensely corroded brecciated and intensely corroded and replaced secondary calcic karstic rocks. The carbon, oxygen and strontium...
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| Published in: | Acta geologica Sinica (Beijing) Vol. 88; no. 6; pp. 1852 - 1862 |
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| Language: | English |
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01-12-2014
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| Abstract | Karst rocks from the Huanglong Formation exposed at the margin of the Eastern Sichuan Basin can be divided into four types：slightly corroded, moderately corroded porous, intensely corroded brecciated and intensely corroded and replaced secondary calcic karstic rocks. The carbon, oxygen and strontium isotope compositions of the various karst rocks are analyzed systematically and compared to rocks without karst corrosion. The results indicate that（1） the Huanglong Formation in the eastern Sichuan Basin was a restricted bay supplied and controlled by freshwater in which mudmicrite and mud-dolomicrite exhibit low δ13C and δ18O values and high 87Sr/86 Sr ratios;（2） all types of karstic rocks in the paleokarst reservoirs of the Huanglong Formation in the research area are affected by atmospheric freshwater with the δ13C and δ18O values and 87Sr/86 Sr ratios in the original formation approaching those of atmospheric freshwater, which reflects ancient hydrological conditions, fluid properties, isotopic source and the fractionation effect;（3） the intensely corroded and replaced secondary limestone is affected by a variety of diagenetic fluids, often reflected by δ13C and δ18O values, while the 87Sr/86 Sr ratios exhibit the strong degree of the corrosion;（4） after comparing the 87Sr/86 Sr ratios of each type of karst rock, the diagenetic fluids are determined to be mainly atmospheric freshwater, and depending on the strength of corrosion, and the low 87Sr/86 Sr ratio fluids in the layer will participate in the karst process. The carbon, oxygen, and strontium isotopes of different karstic reservoirs can provide meaningful geochemical information for forecasting and evaluating the development and distribution rules of the Huanglong Formation at the margin of the eastern Sichuan Basin in time and space. |
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| AbstractList | Karst rocks from the Huanglong Formation exposed at the margin of the Eastern Sichuan Basin can be divided into four types：slightly corroded, moderately corroded porous, intensely corroded brecciated and intensely corroded and replaced secondary calcic karstic rocks. The carbon, oxygen and strontium isotope compositions of the various karst rocks are analyzed systematically and compared to rocks without karst corrosion. The results indicate that（1） the Huanglong Formation in the eastern Sichuan Basin was a restricted bay supplied and controlled by freshwater in which mudmicrite and mud-dolomicrite exhibit low δ13C and δ18O values and high 87Sr/86 Sr ratios;（2） all types of karstic rocks in the paleokarst reservoirs of the Huanglong Formation in the research area are affected by atmospheric freshwater with the δ13C and δ18O values and 87Sr/86 Sr ratios in the original formation approaching those of atmospheric freshwater, which reflects ancient hydrological conditions, fluid properties, isotopic source and the fractionation effect;（3） the intensely corroded and replaced secondary limestone is affected by a variety of diagenetic fluids, often reflected by δ13C and δ18O values, while the 87Sr/86 Sr ratios exhibit the strong degree of the corrosion;（4） after comparing the 87Sr/86 Sr ratios of each type of karst rock, the diagenetic fluids are determined to be mainly atmospheric freshwater, and depending on the strength of corrosion, and the low 87Sr/86 Sr ratio fluids in the layer will participate in the karst process. The carbon, oxygen, and strontium isotopes of different karstic reservoirs can provide meaningful geochemical information for forecasting and evaluating the development and distribution rules of the Huanglong Formation at the margin of the eastern Sichuan Basin in time and space. |
| Author | CHEN Haoru ZHENG Rongcai WEN Huaguo LI Shilin LI Shuang ZHOU Gang WEN Longbin |
| AuthorAffiliation | State Key Laboratory of Oil and Gas Reservoir Geology andExploitation, Chengdu University of Technology, Chengdu 610059, China Chongqing Gas District of Southwest Oil and Gas Company ofCNPC, Chongqing 400021, China Petroleum Exploration and Development Research Institute, PetroChina Southwest Oil and Gasfield Company, Chengdu, 610051, Sichuan China |
| Author_xml | – sequence: 1 givenname: Haoru surname: CHEN fullname: CHEN, Haoru organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation; Chengdu University of Technology; Chengdu 610059 China – sequence: 2 givenname: Rongcai surname: ZHENG fullname: ZHENG, Rongcai organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation; Chengdu University of Technology; Chengdu 610059 China – sequence: 3 givenname: Huaguo surname: WEN fullname: WEN, Huaguo organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation; Chengdu University of Technology; Chengdu 610059 China – sequence: 4 givenname: Shilin surname: LI fullname: LI, Shilin organization: Chongqing Gas District of Southwest Oil and Gas Company of CNPC; Chongqing 400021 China – sequence: 5 givenname: Shuang surname: LI fullname: LI, Shuang organization: Chongqing Gas District of Southwest Oil and Gas Company of CNPC; Chongqing 400021 China – sequence: 6 givenname: Gang surname: ZHOU fullname: ZHOU, Gang organization: Petroleum Exploration and Development Research Institute; PetroChina Southwest Oil and Gasfield Company; 610051 Chengdu Sichuan China – sequence: 7 givenname: Longbin surname: WEN fullname: WEN, Longbin organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation; Chengdu University of Technology; Chengdu 610059 China |
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| Cites_doi | 10.1130/0091-7613(1990)018<0618:ADSPGR>2.3.CO;2 10.1007/BF03175448 10.1111/j.1755-6724.2004.tb00208.x 10.1111/j.1755-6724.2004.tb00182.x 10.1111/j.1755-6724.2002.tb01033.x 10.1016/S0009-2541(99)00081-9 10.1111/j.1755-6724.2012.00715.x 10.1016/0037-0738(71)90016-9 10.1306/12220303072 10.1306/M77973 10.1016/j.sedgeo.2008.10.004 10.1111/j.1365-3091.2008.00960.x 10.1016/0009-2541(93)90131-2 10.1016/S0012-821X(03)00589-2 10.1016/j.chemgeo.2012.03.002 10.1016/j.gexplo.2008.11.005 10.1016/S1876-3804(11)60032-3 10.1016/S1876-3804(09)60107-5 |
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| DocumentTitleAlternate | The Origin of Paleokarst in the Huanglong Formation of the Eastern Sichuan Basin：Evidence from δ~（13）C, δ~（18）O and ~（87）Sr/~（86）Sr |
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| Notes | paleokarst reservoirs,carbon and oxygen isotope,strontium isotope,geochemistry,Huanglong Formation,eastern Sichuan area 11-2001/P Karst rocks from the Huanglong Formation exposed at the margin of the Eastern Sichuan Basin can be divided into four types：slightly corroded, moderately corroded porous, intensely corroded brecciated and intensely corroded and replaced secondary calcic karstic rocks. The carbon, oxygen and strontium isotope compositions of the various karst rocks are analyzed systematically and compared to rocks without karst corrosion. The results indicate that（1） the Huanglong Formation in the eastern Sichuan Basin was a restricted bay supplied and controlled by freshwater in which mudmicrite and mud-dolomicrite exhibit low δ13C and δ18O values and high 87Sr/86 Sr ratios;（2） all types of karstic rocks in the paleokarst reservoirs of the Huanglong Formation in the research area are affected by atmospheric freshwater with the δ13C and δ18O values and 87Sr/86 Sr ratios in the original formation approaching those of atmospheric freshwater, which reflects ancient hydrological conditions, fluid properties, isotopic source and the fractionation effect;（3） the intensely corroded and replaced secondary limestone is affected by a variety of diagenetic fluids, often reflected by δ13C and δ18O values, while the 87Sr/86 Sr ratios exhibit the strong degree of the corrosion;（4） after comparing the 87Sr/86 Sr ratios of each type of karst rock, the diagenetic fluids are determined to be mainly atmospheric freshwater, and depending on the strength of corrosion, and the low 87Sr/86 Sr ratio fluids in the layer will participate in the karst process. The carbon, oxygen, and strontium isotopes of different karstic reservoirs can provide meaningful geochemical information for forecasting and evaluating the development and distribution rules of the Huanglong Formation at the margin of the eastern Sichuan Basin in time and space. |
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| PublicationDate | 2014-12-00 |
| PublicationDateYYYYMMDD | 2014-12-01 |
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| PublicationTitle | Acta geologica Sinica (Beijing) |
| PublicationTitleAlternate | Acta Geologica Sinica |
| PublicationYear | 2014 |
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| Snippet | Karst rocks from the Huanglong Formation exposed at the margin of the Eastern Sichuan Basin can be divided into four types：slightly corroded, moderately... |
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| SubjectTerms | 古岩溶储层 四川盆地东部 地球化学信息 大气淡水 成岩流体 锶同位素 黄龙组 |
| Title | The Origin of Paleokarst in the Huanglong Formation of the Eastern Sichuan Basin：Evidence from δ~（13）C, δ~（18）O and ~（87）Sr/~（86）Sr |
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