石油与天然气地质 ›› 1987, Vol. 8 ›› Issue (4): 424-428.doi: 10.11743/ogg19870415

• 论文 • 上一篇    下一篇

广西来宾吴家坪组生物岩礁

杨万容   

  1. 中国科学院南京地质古生物研究所
  • 收稿日期:1986-07-12 修回日期:1987-06-05 出版日期:1987-12-25 发布日期:2012-01-16

BIOHERM OF WUJIAPING FORMATION IN LAIBIN, GUANGXI

Yang Wanrong   

  1. Nanjing Institute of Geology and Palaeontology, Academia Sinica
  • Received:1986-07-12 Revised:1987-06-05 Online:1987-12-25 Published:2012-01-16

摘要:

广西来宾吴家坪组中段发育的礁体,厚约100m,为陆棚上盆内台地边缘礁。造礁生物为钙质海绵、蓝绿藻和Tabulozoa,Tubiphytes等。含量一般在25—30%,局部可达75%以上;碳酸盐岩色浅质纯,不含燧石及陆源物质,地貌上呈低幅度隆起。以海绵(Tabulozoa)起支撑障积作用,蓝藻起粘结作用的藻、海绵粘结障积岩-藻、海绵粘结骨架岩型的生物岩礁。

Abstract:

Bioherm developed in the middle of the Wujiaping Formation is less than 100 m thick and belongs to marginal reef of intra-basin platform on shelf.The main features of the bioherm are: 1.It is a low range upwarp which is made of white massive rocks within visible lamination. 2.It contains abundant reef-building organisms such as calcisponges, blue-green algae, Tubiphytes, green algae and red algae. The content is usually 25-30%, locally above 75%. 3.It is composed almost completely of pure carbonate rocks without chertsand terrigenous debris. 4.It has a complete facies assemblage of slump microbreccia in reef-front,algae-sponge reef limestone in reef core and gymnocodium micrite in back-reef. The primary reef-building organisms are calcisponges,tabulozoans,Anthraco-porella, blue-green algae and Tubiphytes. The first group organisms are supporting and baffling ones, and the last two are binding and encasing ones.