西南石油大学学报(自然科学版) ›› 1984, Vol. 6 ›› Issue (4): 19-32.DOI: 10.3863/j.issn.1000-2634.1984.04.002

• 论文 • 上一篇    下一篇

四川重庆北碚地区上二叠统文星场礁的岩石学及微相特征

腾杰
  

  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:1984-11-20 发布日期:1984-11-20

PETROLOGY AND MICROFACIES OF ORGANIC REEFS IN BEIBEI,CHONGQING, SICHUAN

Teng Jie   

  • Received:1900-01-01 Revised:1900-01-01 Online:1984-11-20 Published:1984-11-20

摘要: 重点讨论了四川重庆北碚天府地区上二叠统生物礁的岩石类型,生物礁组合的微相特征和发育演化史。微相组合和生物学特征证明文星场生物礁是发育在开放性泻湖中的点礁,它的生长、发育受沉积速率控制,消亡的原因是由于海平面的上升速度超过礁的生长速度。

Abstract:

We have found five organic reef bodies in the same strata and I the same area since we discovered an organic reef in the strata of the Upper Permian in Beibei of Sichuan Province in 1983. We have mainly discussed one of the bodies, named Wenxin Reef In this paper. According to its paleo-biological nature and microfacies character, we have proposed that it is a kind of patch reef developed in an open lagoon. The patch reef sedimentary assemblages include:
1. reef-core subfacies;
2. reef-flank subfacies;
3. inter-reef subfacies.
Its development underwent four stages: beginning to grow in the sea-up-shallowing, and then withering in the sea-up-deepening.