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鄂西利川见天坝长兴组海绵礁岩石类型及礁体演化阶段
引用本文:王延奇,胡明毅,刘富艳,王辉,胡治华. 鄂西利川见天坝长兴组海绵礁岩石类型及礁体演化阶段[J]. 岩性油气藏, 2008, 20(3): 44-48
作者姓名:王延奇  胡明毅  刘富艳  王辉  胡治华
作者单位:1. 长江大学油气资源与勘探技术教育部重点实验室
2. 长江大学油气资源与勘探技术教育部重点实验室;中海油天津分公司
摘    要:鄂西利川见天坝长兴组生物礁位于镶边型台地陡斜的边缘上,濒临鄂西海槽,属于台地边缘礁。该礁体的最大特点是大型柱状海绵丰富,构成生物骨架。生物礁岩石类型主要有障积岩、障积-骨架岩、骨架岩、粘结岩、角砾状灰岩5种。通过分析见天坝生物礁的生物类型、岩石宏观类型和特征,推测生物礁的发展演化经历了5个阶段:奠基期、拓殖期、泛殖期、衰亡期和礁盖期。

关 键 词:生物礁  发展演化  长兴组  见天坝

Rock types and evolution of reef of Changxing Formation in Jiantianba of western Hubei
WANG Yan-qi,HU Ming-yi,LIU Fu-yan,WANG Hui,HU Zhi-hua. Rock types and evolution of reef of Changxing Formation in Jiantianba of western Hubei[J]. Northwest Oil & Gas Exploration, 2008, 20(3): 44-48
Authors:WANG Yan-qi  HU Ming-yi  LIU Fu-yan  WANG Hui  HU Zhi-hua
Affiliation:WANG Yan-qi, HU Ming-yi, LIU Fu-yan, WANG Hui, HU Zhi-hua ( 1. Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Jingzhou 434023, China; 2. Tianjin Branch, CNOOC, Tianjin 300452, China)
Abstract:Being located in the margin of platform and close to Western Hubei Trough, reef of Changxing Formation in western Hubei is a kind of platform marginal reef. The reefs have abundant large scale of cylindric sponges which compose the organic framework. There are mainly five types of rocks, including bafflestone, bafflestone-framestone, framestone, bindstone and breceiform limestone. Based on the analysis of the types of reefs and rocks, it is supposed that the evolution of the reef experienced five stages: foundation stage, pioneering stage, flourishing stage, decline stage and reef cap stage.
Keywords:reef  evolution  Changxing Formation  Jiantianba
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