Research history and progress on reflux seepage dolostone
Yuan Xinpeng1, Liu Jianbo1,2,3
1 School of Earth and Space Sciences，Peking University，Beijing 100871 2 Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education，Peking University,Beijing 100871 3 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, Jiangsu
Abstract Reflux seepage dolostones were widely distributed in the geological records and considered to be potential high-quality reservoirs of applicable value.Recent studies on the reflux model of dolomitization highlight its advances and controversies.This paper briefly covers the research history and progress of the brine reflux model and its application.The source of magnesium，the fluid-flow mechanism and the ancient characteristics of rocks in this model are particularly summarized.Some new researches such as penesaline dolomitization by reflux seepage provide a new impetus to revisit the primary model.
About author: Yuan Xinpeng，born in 1985，is a Ph.D.candidate of paleontology and stratigraphy.E-mail: yuanxinpeng2011@hotmail.com. About the corresponding author Liu Jianbo，born in 1966，is engaged in paleontology，sedimentology，and paleoenvironment changes.E-mail:jbliu@pku.edu.cn.
Cite this article:
Yuan Xinpeng,Liu Jianbo. Research history and progress on reflux seepage dolostone[J]. JOURNAL OF PALAEOGEOGRAPHY, 2012, 14(2): 219-228.
Yuan Xinpeng,Liu Jianbo. Research history and progress on reflux seepage dolostone[J]. JOPC, 2012, 14(2): 219-228.
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