Dolomitization of felsic volcaniclastic rocks in continental strata: A study from the Lower Cretaceous of the A'nan Sag in Er'lian Basin, China
Dolomitization of fine-grained volcaniclastic rocks is common in the Lower Cretaceous of the A'nan Sag in the Er'lian Basin of China. Analysis of core samples shows that the organic-rich volcaniclastic rocks are mainly composed of reworked felsic volcanic materials and terrigenous clay min...
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Published in | Sedimentary geology Vol. 353; pp. 13 - 27 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
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Elsevier B.V
15.05.2017
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Abstract | Dolomitization of fine-grained volcaniclastic rocks is common in the Lower Cretaceous of the A'nan Sag in the Er'lian Basin of China. Analysis of core samples shows that the organic-rich volcaniclastic rocks are mainly composed of reworked felsic volcanic materials and terrigenous clay minerals. The fine-grained volcaniclastic rocks can be divided into four types: volcaniclastic rocks without carbonatization, volcaniclastic rocks with ferroan dolomites, dolomitized and calcified volcaniclastic rocks, and calcified volcaniclastic rocks. The parent rocks of the volcaniclastic rocks have high silicon and potassium contents and low iron and magnesium contents, and are probably felsic magma of the calc-alkaline series. The average values of δ13CPDB of the carbonate minerals are about 3.13‰; the average values of δ18OPDB are about −16.74‰. The compositions of C and O isotopes are probably influenced by bacterial methanogenesis. Iron, magnesium, and calcium are probably derived from illitization of terrigenous smectite. A model for dolomitization of felsic volcaniclastic rock is proposed, including three stages: 1) mixed sedimentation and bacterial methanogenesis (<75°C); 2) transformation of clay minerals (>70°C) and dolomitization (75 to 97°C); and 3) dissolution. Late dissolution of authigenic carbonate minerals, creating abundant secondary pores, is significant for hydrocarbon accumulation. |
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AbstractList | Dolomitization of fine-grained volcaniclastic rocks is common in the Lower Cretaceous of the A'nan Sag in the Er'lian Basin of China. Analysis of core samples shows that the organic-rich volcaniclastic rocks are mainly composed of reworked felsic volcanic materials and terrigenous clay minerals. The fine-grained volcaniclastic rocks can be divided into four types: volcaniclastic rocks without carbonatization, volcaniclastic rocks with ferroan dolomites, dolomitized and calcified volcaniclastic rocks, and calcified volcaniclastic rocks. The parent rocks of the volcaniclastic rocks have high silicon and potassium contents and low iron and magnesium contents, and are probably felsic magma of the calc-alkaline series. The average values of δ13CPDB of the carbonate minerals are about 3.13‰; the average values of δ18OPDB are about −16.74‰. The compositions of C and O isotopes are probably influenced by bacterial methanogenesis. Iron, magnesium, and calcium are probably derived from illitization of terrigenous smectite. A model for dolomitization of felsic volcaniclastic rock is proposed, including three stages: 1) mixed sedimentation and bacterial methanogenesis (<75°C); 2) transformation of clay minerals (>70°C) and dolomitization (75 to 97°C); and 3) dissolution. Late dissolution of authigenic carbonate minerals, creating abundant secondary pores, is significant for hydrocarbon accumulation. |
Author | Jia, Ye Wei, Wei Yue, Hui Zhu, Xiaomin Liu, Xin Zhu, Shifa Sun, Shuyang |
Author_xml | – sequence: 1 givenname: Shifa surname: Zhu fullname: Zhu, Shifa email: zhushifa_zsf@163.com organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 2 givenname: Hui surname: Yue fullname: Yue, Hui organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 3 givenname: Xiaomin surname: Zhu fullname: Zhu, Xiaomin organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 4 givenname: Shuyang surname: Sun fullname: Sun, Shuyang organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 5 givenname: Wei surname: Wei fullname: Wei, Wei organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 6 givenname: Xin surname: Liu fullname: Liu, Xin organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China – sequence: 7 givenname: Ye surname: Jia fullname: Jia, Ye organization: State Key Laboratory of Petroleum Resources and Prospecting, Beijing 102249, China |
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Keywords | Ferroan dolomite A'nan Sag Volcaniclastic rock Dolomitization Felsic volcanic materials Er'lian Basin |
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SubjectTerms | A'nan Sag Dolomitization Er'lian Basin Felsic volcanic materials Ferroan dolomite Volcaniclastic rock |
Title | Dolomitization of felsic volcaniclastic rocks in continental strata: A study from the Lower Cretaceous of the A'nan Sag in Er'lian Basin, China |
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