Mineralogical correlation between primary and replacement dolomites
Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogieal study the indicators for correlation between the primary dolomites which are not influenced by the diagenesis and the replacement dolomites of different periods have been obtained. It is shown that the primary do...
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| Published in | Science China. Earth sciences Vol. 40; no. 1; pp. 91 - 98 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Dordrecht
Springer Nature B.V
01.02.1997
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| Subjects | |
| Online Access | Get full text |
| ISSN | 1674-7313 1006-9313 1869-1897 1862-2801 |
| DOI | 10.1007/BF02878585 |
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| Abstract | Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogieal study the indicators for correlation between the primary dolomites which are not influenced by the diagenesis and the replacement dolomites of different periods have been obtained. It is shown that the primary dolomites are characterized by crystal forms precipitated and deposited directly from sea water, stable and homogeneous distribution of Mg and Ca, ideal chemical composition, regular modulated microstructures, low positive δ13C and low negative δ18O. |
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| AbstractList | Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogical study the indicators for correlation between the primary dolomites which are not influenced by the diagenesis and the replacement dolomites of different periods have been obtained. It is shown that the primary dolomites are characterized by crystal forms precipitated and deposited directly from sea water, stable and homogeneous distribution of Mg and Ca, ideal chemical composition, regular modulated microstructures, low positive delta super(13)C and low negative delta super(18)O. Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogieal study the indicators for correlation between the primary dolomites which are not influenced by the diagenesis and the replacement dolomites of different periods have been obtained. It is shown that the primary dolomites are characterized by crystal forms precipitated and deposited directly from sea water, stable and homogeneous distribution of Mg and Ca, ideal chemical composition, regular modulated microstructures, low positive δ13C and low negative δ18O. Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogical study the indicators for correlation between the primary dolomites which are not influenced by the diagenesis and the replacement dolomites of different periods have been obtained. It is shown that the primary dolomites are characterized by crystal forms precipitated and deposited directly from sea water, stable and homogeneous distribution of Mg and Ca, ideal chemical composition, regular modulated microstructures, low positive δ13C and low negative δ18O. |
| Author | 黄志诚 杨守业 陈智娜 |
| AuthorAffiliation | Department of Earth Sciences Nanjing University Nanjing 210093 China China |
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| CitedBy_id | crossref_primary_10_1016_j_marpetgeo_2019_01_016 crossref_primary_10_1007_BF02893783 crossref_primary_10_1007_s11430_013_4654_x crossref_primary_10_1111_1755_6724_13459 crossref_primary_10_1016_j_quaint_2020_02_018 crossref_primary_10_1007_s11430_011_4356_1 crossref_primary_10_1016_j_precamres_2020_105694 |
| Cites_doi | 10.1007/BF00429430 10.1130/0091-7613(1985)13<457:CTICD>2.0.CO;2 |
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| Copyright | Science in China Press 1997. |
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| References | Wang Yinghua (BF02878585_CR3) 1991 R. J. Reeder (BF02878585_CR8) 1993; 27 Wang Yinghua (BF02878585_CR2) 1987; 5 D. E. Miser (BF02878585_CR6) 1987; 72 H. R. Wenk (BF02878585_CR9) 1985; 13 H. Blatt (BF02878585_CR1) 1980 H-R. Wenk (BF02878585_CR5) 1983; 11 D. W. Morrow (BF02878585_CR4) 1982; 9 D. J. Barber (BF02878585_CR7) 1985; 91 |
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| Snippet | Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogieal study the indicators for correlation between the primary dolomites... Primary dolostones occur in the Upper Sinian Dengying Formation. Based on mineralogical study the indicators for correlation between the primary dolomites... |
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| SubjectTerms | Chemical composition China Correlation Crystals Dengying Deposition Diagenesis Dolomite Formation Geochemistry Indicators Marine Microstructure Mineralogy primary replacement Sea water Seawater |
| Title | Mineralogical correlation between primary and replacement dolomites |
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