Paleozoic and Cenozoic Reef Formation. An Attempt at Comparative Analysis

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
V. G. Kuznetsov
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引用次数: 0

Abstract

The article presents a comparative analysis of the Paleozoic and Cenozoic reef formation, mainly in terms of the position of reefs in the basins of continental and oceanic blocks. It is shown that the main formation of reefs took place in the Cenozoic directly in the oceans, including boundaries between oceans and continents, and, to an extremely limited scales, in the basins of the continental segment. In the Paleozoic, reefs were formed not only in oceans, but also in spacious basins of continental block. This is one of the manifestations of the general evolution of carbonate accumulation, when the Paleozoic carbonate sediments were formed in such shallow-water bodies that covered very significant surfaces of continents.

Abstract Image

Abstract Image

古生代和新生代岩礁形成。比较分析尝试
摘要 文章对古生代和新生代珊瑚礁的形成进行了比较分析,主要从珊瑚礁在大陆块和大洋块盆地中的位置进行了分析。结果表明,在新生代,珊瑚礁的主要形成直接发生在海洋中,包括海洋和大陆之间的边界,以及在极其有限的范围内,发生在大陆段的盆地中。在古生代,珊瑚礁不仅在海洋中形成,也在宽敞的大陆块盆地中形成。这是碳酸盐累积总体演化的表现之一,当时古生代碳酸盐沉积物形成于覆盖大陆重要表面的浅水体中。
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来源期刊
Lithology and Mineral Resources
Lithology and Mineral Resources 地学-地球化学与地球物理
CiteScore
1.30
自引率
37.50%
发文量
29
审稿时长
>12 weeks
期刊介绍: Lithology and Mineral Resources is an international peer reviewed journal that publishes articles on a wide range of problems related to the formation of sedimentary rocks and ores. Special attention is given to comparison of ancient sedimentary rock and ore formation with present-day processes. The major part of the journal is devoted to comparative analysis of sedimentary processes on the continents and in oceans, as well as the genetic aspects of the formation of sedimentary and hydrothermal–sedimentary mineral resources. The journal welcomes manuscripts from all countries in the English or Russian language.
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