摘要
桂林地区丰富多采的上泥盆统藻礁灰岩形成于台地边缘相。本文介绍两个别具风格的藻礁——奇峰镇葵盘石—藻礁和寨江藻礁,并从区域沉积相、造架生物和碳酸盐岩石学等方面对藻礁进行较详细的论述。
A great variety of Upper Devonian algal reef limestones in the Guilin area, Guangxi,were formed in the platformmargin facies. This paper mainly introduces two salient algal reefs and discusses the paleogeographical setting of reef building. The Qifengzhen receptaculites-alga reef was formed at the end of the Frasnian (Late Devonian). The reef body is 33m thick and 150m long. The reef-building organisms include receplacuites, blue, red algae and compound tetracorals. The rocks belong to the lind-framework type and lind-laffle type. According to the characteristics of lateral lithological changes of organic reefs. the reef facies may be divided into reef core, reef front and back-reef subfacies. The Zhai jiang algal reef was formed in the Famennian Stage(Late Devonian). It is composed of renalcids and Epiphyton, 43m thick and 60m long. The rocks belong to the baffle-framework type and lind type. The Zhai jiang algal reef occurs as an isolated knoll; its surroundings have been denuded and only the reef core subfacies and reef base remain now.
出处
《中国区域地质》
CSCD
1990年第4期334-338,T001,共6页
Regional Geology of China
