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Zhou Zhengyi, Liu Dehan, Sheug Guoying. GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA[J]. Acta Sedimentologica Sinica, 1983, 1(2): 143-152.
Citation: Zhou Zhengyi, Liu Dehan, Sheug Guoying. GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA[J]. Acta Sedimentologica Sinica, 1983, 1(2): 143-152.

GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA

  • Received Date: 1982-09-17
  • Publish Date: 1983-06-10
  • In this paper the paleotemperature in the BZ area of Tarim Basin is studi一ed and its geological model is temperature at lhc end of the made.There was a local thermal alteration at high Paleozoic as a result of a large scale igneous ro-ck intrusion, w hereas the gradients of paleotem peratures of the tum and Cenozoic stratum are lower in this area.Although Mesozoic sira-crude oil from Z一1 well is produced from the lower Carboniferous system, its source rock seems to be middle一upper Carboniferous carbonate distributed in the southern BZ area.The result calculated from TTf value shows that the source roc's Su-tied within 3000-6000 metre deep are still at their main oil一forming stage.
  • [1] (1)周中毅等,(1919)碳酸盐岩中有机质的热变实验。中国科学院地球化学研究听年报, 1978-197 9),66-68页。

    (2)郝石生,(1982)华北地区震旦亚界古地温演化及冀中地1原生油气藏形成条件初探,华东石油学院学报,1,1-170

    (3) 张子枢,(1980)成熟度的化学及矿物学指标分类,地质地球化学,922-290

    (4) 浅川忠(1979)泥质岩 -碳酸盐岩沉积阶段和油气的生成、运移、聚集与压实特征之间的关系,石油地质实验,4,1-220

    (5) Waples, D.W.,(1980)Time and Temperature in Petroleum Formation:Application of Lopatin's Method to Petroleum Exploration, BuII.AAPG.V.64 N.6

    (6) Tissot,B.B.,and Welte, D.H.,(1978)Petroleum Formation and Occurre-nce, Nnw York

    (7) Cooper, B.S·,(1977)Estimaiion of the Rlasimum Temperatures Attained in Sedimeniary一Rock,Dcvclopments in Petrolcun Geology-I, London,Applied Science Pub.

    (8) Connan, J.,(1974)Time一Temperature Relation in Oil Genesis,Bull.AAPG,V.58 N.12

    (9)Hood, J·,et al.,(1975)Organic Metamorphism and the Generation of Petr-oleum, Bull.AAPG.V. 59N.6

    (10)Veto, I.,(1979)An Exmination of the Timing of Catagenesis of Organic Matter Using Three Published Methods ,Advarrces in Organic Gcochcmistry
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  • Received:  1982-09-17
  • Published:  1983-06-10

GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA

Abstract: In this paper the paleotemperature in the BZ area of Tarim Basin is studi一ed and its geological model is temperature at lhc end of the made.There was a local thermal alteration at high Paleozoic as a result of a large scale igneous ro-ck intrusion, w hereas the gradients of paleotem peratures of the tum and Cenozoic stratum are lower in this area.Although Mesozoic sira-crude oil from Z一1 well is produced from the lower Carboniferous system, its source rock seems to be middle一upper Carboniferous carbonate distributed in the southern BZ area.The result calculated from TTf value shows that the source roc's Su-tied within 3000-6000 metre deep are still at their main oil一forming stage.

Zhou Zhengyi, Liu Dehan, Sheug Guoying. GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA[J]. Acta Sedimentologica Sinica, 1983, 1(2): 143-152.
Citation: Zhou Zhengyi, Liu Dehan, Sheug Guoying. GEOLOGICAL MODEL OF PALEOTEMPERATURE AND CALCULATION OF OIL GENERATION PER旧D!N THE BZ AREA[J]. Acta Sedimentologica Sinica, 1983, 1(2): 143-152.
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