西南石油大学学报(自然科学版) ›› 1995, Vol. 17 ›› Issue (4): 1-5.DOI: 10.3863/j.issn.1000-2634.1995.04.001

• 石油地质勘探 •    下一篇

塔里木盆地震旦纪—奥陶纪岩相古地理

郑家凤 穆曙光
  

  1. 石油勘探系
  • 收稿日期:1995-05-05 修回日期:1900-01-01 出版日期:1995-11-20 发布日期:1995-11-20

Sinian—Ordivieian Dithfaeies PaleogeograPhy of Tarim Basin

Zheng Jia-feng Mu Shu-guang
  

  1. Department of oil exploration
  • Received:1995-05-05 Revised:1900-01-01 Online:1995-11-20 Published:1995-11-20

摘要: 衰旦纪至早古生代中期(寒式纪、奥淘纪),差异性构造升降活动,使塔里木盆地的古地
理格局岌生丁重大演化.襄旦纪,盆地性质具滨、浅海及局限海盆特征,寒式纪,盆地古地理特征的总趁势足西高东低,依次为破酸盆台地-针坡-深海盆地,奥内纪,大规模海俊使中-西那的破酸盆台地转化为混积法栩,深海盆地也由寒武纪时期的欠补偿性演化为奥沟纪的补偿性盆地。到晚奥内世晚期,早加里东运动的影响,海水凡乎全邵退出塔里木盆地,结未了盆地范围内衷旦纪~奥内纪沉积古地理发展演化史。

关键词: 沉积岩相, 古地理环境, 构造运动, 塔里盆地

Abstract:

Tarim basin is a composite basin with multiple cycles. As the first set of sedimentary cover on the basement,Sinian,Cambrian and Ordivician systems are charaeterized by great thickness and abundant sedimentary types. Lithofacies paleogeographic environment stretches from seastrand to deep sea. Basing on the outcrop seetion,drilling data and the analysis of
carbon-oxygen isotope,trace element, geoehemistry and palaeontology,the feature and distribution of lithofacies paleogeograpic environment in Sinian,Cambrian and Ordivieian periods are analyzed in this paper.

Key words:

Paleogeographic envionment

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