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Cambrian Reefs in the Western North China Platform, Wuhai, Inner Mongolia

Cited 2 time in scopus
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Title
Cambrian Reefs in the Western North China Platform, Wuhai, Inner Mongolia
Other Titles
북중국대지 서부 (내몽고 우하이 지역)의 캠브리아기 생물초
Authors
Lee, Jeong-Hyun
Woo, Jusun
Lee, Dong-Jin
Choh, Suk-Joo
Park, Tae-Yoon S.
리앙쿤
김병준
Subject
Geology
Keywords
Cambrian; Reef; microbialite; siliceous sponge; western North China Platform
Issue Date
2016
Citation
Lee, Jeong-Hyun, et al. 2016. "Cambrian Reefs in the Western North China Platform, Wuhai, Inner Mongolia". ACTA GEOLOGICA SINICA-ENGLISH EDITION, 90(6): 1946-1954.
Abstract
Cambrian thrombolites and maze-like maceriate reefs are reported from the western North China Platform, Wuhai, Inner Mongolia, China. Both types of reef occur in the middle of a succession dominated by thin-bedded lime mudstone-shale/marlstone alternations, and are laterally surrounded by limestone conglomerate and/or grainstone. Thrombolite, characterized by meter-scale lenticular mounds composed of millimeter- to centimeter-scale mesoclots and wackestone matrix, occurs in the lower middle part of the sequence. Thrombolite mesoclots are composed of microstromatolites with alternating dark gray and light gray micritic laminae. The maze-like maceriate reefs occur in the middle to the upper part of the sequence, commonly forming lenticular mounds up to 1 m thick. They are characterized by centimeter- to decimeter-scale branched maze-like structures, whose biogenic portions (maceria) are selectively dolomitized. The maceriae are composed of poorly preserved microstromatolites and siliceous sponges. Inter-macerial sediments consist of lime mud and scattered bioclasts. These Wuhai reefs are generally similar to various Cambrian reefs previously reported from Shandong region, China.
URI
http://repository.kopri.re.kr/handle/201206/6402
DOI
http://dx.doi.org/10.1111/1755-6724.13014
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