石油与天然气地质 ›› 1993, Vol. 14 ›› Issue (2): 98-105.doi: 10.11743/ogg19930202

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鄂尔多斯东南缘奥陶系碳酸盐岩成岩温度

叶俭1, 云琼英2, 胡显穆2   

  1. 1. 西安地质学院 710054;
    2. 华北石油地质局第三普查勘探大队 陕西 咸阳712000
  • 收稿日期:1991-12-06 修回日期:1992-07-13 出版日期:1993-06-25 发布日期:2012-01-16
  • 基金资助:

    国家“七五”重点攻关项目54-01-09-03

DIAGENETIC TEMPERATURE OF ORDOVICIAN CARBONATE ROCK IN SOUTHEAST MARGIN OF ORDOS

Ye Jian1, Yun Qunying2, Hu Xianmu2   

  1. 1. Xian Institute of Geology;
    2. 3rd Brigade of Petroleum Exploration and Prospecting, North China Bureau of Petroleum Geology
  • Received:1991-12-06 Revised:1992-07-13 Online:1993-06-25 Published:2012-01-16

PDF (PC)

721

被引次数

10

摘要：

鄂尔多斯东南缘奥陶系溶洞充填物的流体包裹体和稳定同位素研究,得到了四个不连续温度系列,其中44—46℃、59—61℃、104—118℃为加里东期,156—169℃为海西期。据此,可以认为下奥陶统的有机质在加里东期已达成熟,在海西期转化为气。根据下奥陶统马家沟组底部的流体包裹体均一温度资料和盆地周边中、上奥陶统较深水特征,鄂尔多斯中部曾接受过中、上奥陶统沉积,在加里东运动后方被剥蚀。

关键词: 鄂尔多斯, 奥陶系, 流体包裹体, 古地温, 溶洞, 油气演化

Abstract:

Studied the fluid inclusions and stable isotopes in the fillings of Lower Paleozoic dissolve burrows on the southeast margin of Ordos,four discontinuous temperature sequences were recovered:44—46℃,59—61℃ and 104—118℃ were Caledonian orogenic stage,156—169℃ was Hercynian orogenic stage.Therefore,it might be considered that organic matter of Lower Ordovician was mature in Caledonian stage and turned into gas in Her-cynian.According to the paleotemperature of the bottom of Majiagou Formation in LowerOrdovician and the deep water characters of Middle-Upper Ordovician on the basin periphery,it is suggested that the internal basin had received Middle-Upper Ordovician sediments which were eroded after Caledonian orogeny.