Geochemical evidence of an oceanic provenance of cherts in accretionary complexes in the Sikhote Alin

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• 作者：I. V. Kemkin ; R. A. Kemkina
• 关键词：geochemistry ; REE ; radiolarian chert ; sedimentation environments ; Sikhote Alin
• 刊名：Geochemistry International
• 出版年：2015
• 出版时间：August 2015
• 年：2015
• 卷：53
• 期：8
• 页码：700-712
• 全文大小：1,600 KB
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  A. I. Khanchuk and I. V. Panchenko, ?
• 作者单位：I. V. Kemkin (1) (2)
  R. A. Kemkina (1) (2)
  
  1. Far East State University, ul. Sukhanova 8, Vladivostok, 690950, Russia
  2. Far East Geological Institute, Far East Branch, Russian Academy of Sciences, pr. Stoletiya Vladivostoka 159, Vladivostok, 660022, Russia
  
• 刊物主题：Geochemistry;
• 出版者：Springer US
• ISSN：1556-1968

文摘

The paper reports pioneering data on the distribution of REE in cherts in the Taukha terrane of the Late Jurassic–Early Cretaceous accretionary prism in the Sikhote Alin and a calculated value of the Ce anomaly. The values of the Ce anomaly, the ratios of certain major components, and the ratios of these components and REE are used to estimate the facies environments in which the cherty material was accumulated. This material is proved to have started accumulating within a zone adjacent to the spreading ridge and continued on the abyssal plane. The uppermost portion of the vertical section, which is made up of siliceous mudstone, was deposited in the marginal part of the paleoocean adjacent to the continental marginal sedimentation region. The sedimentation environments systematically alternating in a single geologic section suggest that the part of the seafloor on which the cherty sediments were accumulated moved from the spreading cen-ter to the margin of the paleocontinent, and this caused the drift of the stratigraphic section across various oceanic facies zones.