石油与天然气地质 ›› 1993, Vol. 14 ›› Issue (4): 285-290.doi: 10.11743/ogg19930404

• 论文 • 上一篇    下一篇

湖北南漳中三叠统巴东组碳酸盐与陆源碎屑混合沉积

王宝清, 胡明毅, 胡爱梅, 陈建明   

  1. 江汉石油学院 湖北 江陵434102
  • 收稿日期:1993-03-01 修回日期:1993-05-27 出版日期:1993-12-25 发布日期:2012-01-16

MIXED CARBONATE-TERRIGENOUS CLASTIC SEDIMENTS OF MIDDLE TRIASSIC BADONG FORMATION IN NANZHANG, HUBEI

Wang Baoqing, Hu Mingyi, Hu Aimei, Chen Jianming   

  1. Jianghan Petroleum Institute, Jiangling, Hubei
  • Received:1993-03-01 Revised:1993-05-27 Online:1993-12-25 Published:2012-01-16

摘要:

湖北南漳中三叠统巴东组是一套碳酸盐与陆源碎屑混合沉积,属低能的潮坪-泻湖环境。表现为下列七种形式:(1)碎屑岩与灰岩互层,(2)碎屑岩夹灰岩,(3)灰岩夹碎屑岩,(4)碳酸盐在碎屑岩中呈胶结物,(5)陆源碎屑散布于碳酸盐基质中,(6)陆源粉砂充填于砾屑灰岩的砾屑之间,(7)碳酸盐颗粒散布于陆源泥中。

关键词: 碳酸盐岩, 陆源碎屑, 混合沉积, 潮坪泻湖, 巴东组

Abstract:

The Middle Triassic Badong Formation,situated in Nanzhang,Hubei Province,is a set of mixed carbonate-terrigenous clastic sediments deposited mainly in a low energy tidal flat-lagoon environment.The sediments occurred in following seven types:1.lime-stone-clastic rocks interbeds;2.clastic rocks intercalated with limestons;3.limestones intercalated with clastic rocks;(4).carbonate appeared as cement in clastic rocks;5.terri-genous clastics distributed in carbonate matrix;6.terrigenous silts filled in pores of intra-clastic limestone;7.carbonate intraclasts distributed in terrigenous mud.