扬子地区奥陶系碳酸盐岩氧、碳同位素与成岩作用  

ON THE RELATIONSHIP BETWEEN THE OXYGEN AND CARBON ISOTOPES AND THE DIAGENESES OF ORDOVICIAN CARBONATE ROCKS IN THE YANGTAC AREA

作　　者：杨长庚 

机构地区：[1]地矿部石油地质中心实验室

出　　处：《石油实验地质》1994年第3期267-273,共7页Petroleum Geology & Experiment

摘　　要：本文通过扬子地区奥陶系１１个剖面的泥晶灰岩δ￣（１８）Ｏ和伴生泥岩沥青的回归计算拟合结果，表明埋藏古地温主导泥晶灰岩氧同位素交换的现象，并借助这种交换结果，讨论了扬子碳酸盐台地区６个剖面点的奥陶系碳酸盐岩在不同成岩环境下６种成岂作用的氧碳同位素特征，此外，依据这些讨论结果，提出了在评价有机质成熟度、油气的储集和运移方面的地质意义。Through the regressional calculation and simulation on theδ￣(18)O of micritic limestoneand of associated argillous asphaltum from the 11 Ordovician sections in the YangtzeArea,it is suggested that the oxygen isotopic exchanges of the micritic limestones shouldbe dominated by buried paleo-geotemperature, Based on the above analysis,the author ofthis paper discusses on the oxygen and carbon isotopic characteristics of the 6 kinds of dia-geneses with different diagenetic environments in the Ordovician carbonate rocks of the 6section points of the Yangtze carbonate platform. Furthermore,the author suggests thegeological significance of the discussions in the assessment on the maturity of organic mat-ter and oil/gas accumulation , preservation,and migration.

关 键 词：奥陶系 成岩作用 奥陶纪 碳酸盐岩 

分 类 号：P618.130.1[天文地球—矿床学]