摘要
新发现的藻－海绵礁产于下奥陶统分乡组上部，时代相当于Ｔｒｅｍａｄｏｃｉａｎ晚期。与礁有关的主要为碳酸盐颗粒岩、泥岩等岩相。沉积层序表明藻－海绵礁是一个由浅变深的演化序列，以沙浪底形为礁基，并在生长过程中强化了此一形态。粘结、障积作用为主，构成Ｃａｌａｔｈｉｕｍ－藻群落；藻－Ｐｕｌｃｈｒｉｌａｍｉｎａ－Ａｒｃｈａｅｏｓｃｙｐｈｉａ群落。
Algal--sponge reefs have been discovered recently in the upper part of the Lower Ordovician Fengxiang Formation, and their age corresponds to Late Tremedocian. The reefs consist mainly grainstone, mudstone,boundstone and bafflestone. The depositional sequence of the algal--sponge reefs suggests a evolution series starting from shallow to deep. The reefs grew on relief bases, and then enhanced the initial forms of the bases as they grew. Bounding and baffling were the main factors in the formation of Calathium--algal and algal--PulchrilaminaArchaeoscyphia communities.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
1995年第4期319-323,共5页
Oil & Gas Geology
基金
国家自然科学基金
