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专辑
网络首发:1990-12-25,
纸质出版:1990
移动端阅览
湖北松滋早奥陶世生物礁为笔者首次发现。可分为藻岩隆礁、叠层石层礁和灰泥岩隆礁。最有代表性的藻岩隆礁由一系列丘状、面包状和似层状礁体组成。单个礁体高1.5—22m
宽6—50m
高/宽比变化于1:3.6—1:4.5间。原地生长的主要造礁生物为蓝绿藻、托盘藻、古钵海绵和少量苔藓虫、钙质海绵。附礁生物为头足类、腕足类、三叶虫、海百合、瓣鳃类、介形虫等。一个完整的礁体由礁基、礁核、礁盖层和礁间沉积物组成。礁核从底到顶可分出三个微相:(1)粘结岩
(2)障积-粘结岩
(3)粘结-障积岩。与此相应
礁体存在三个发展期:奠基期、发育期和衰亡期。
Early Ordovician organic reefs in Songzi were firstly discovered by the authors.The reefs can be divided into algal buildup reef
stromatolite beded reef and lime-mud buildup reef
of which the algal buildup reef is best represented and composed of a series of mound
bread-like
beded-like reef bodies.Individual reef bodies are 1.5-22m high
6-50m wide
and the ratio of high/wide is 1:3.6-1:4.5.The main reef-building or-ganisms in situ are blue-green algae
recept aculitid algae
sponges and a few bryozoans.The accessory organisms are cephalopods (Hopecicoceras
Cameroceras)
brachiopods
trilo-bites
echinoderms
bivalves
ostracods
etc.A complite reef body consists of reef base
reef core
reef cap
and interreef sedi-ments.The reef core can be divided into three microfacies from bottom to top:1.bind-stone
2.baffle-bindstone
3.bind-bafflestone.Correspondingly
the development of the reef bodies can be divided into three periods:foundation stage
development stage and decline stage.
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