Litho- and bio-facies of carbonate sedimentary rocks
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Published by Palaeontological Society of Japan in [Tokyo] .
Written in English

Subjects:

  • Rocks, Carbonate -- Congresses,
  • Petrology -- Asia -- Congresses

Book details:

Edition Notes

Statementedited by Tatsuro Matsumoto.
SeriesPalaeontological Society of Japan special papers -- no. 14
ContributionsMatsumoto, Tatsurō, 1913-
Classifications
LC ClassificationsQE475 L5
The Physical Object
Pagination82p.
Number of Pages82
ID Numbers
Open LibraryOL17898157M

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This textbook provides an overview of the origin and preservation of carbonate sedimentary rocks. The focus is on limestones and dolostones and the sediments from which they are derived. The approach is general and universal and draws heavily on fundamental discoveries, arresting interpretations, and keystone syntheses that have been developed over the last five by: Carbonate rocks (limestones and dolomites) constitute a major part of the geological column and contain not only 60% of the world's known hydrocarbons but also host extensive mineral deposits. This book represents the first major review of carbonate sedimentology since the mid 's.4/5(5).   Middle Triassic carbonates extend from the North-Central Coast region of Vietnam to northern Laos. We conducted sedimentological, paleontological, and geochemical analyses on the carbonates of the Hoang Mai Formation in Nghe An province, Vietnam. The carbonates consist of the following six lithostratigraphic units (from bottom to top): sandy limestone (unit 1), peloidal packstone Author: Thuy Thi Nhu Ha, Hideko Takayanagi, Katsumi Ueno, Yoshihiro Asahara, Koshi Yamamoto, Yasufumi Iryu. The carbonate sediments of central Hokkaido and Miyako, although almost coeval, are clearly different from each other in litho- and biofacies. Sano () described a coral-rudist limestone in the Miyako Group. The limestone is small in scale (about 50 m x 20 m x 1 m) and occurs directly on the basement by:

This textbook outlines the physical, chemical, and biologic properties of the major sedimentary rocks, as revealed by petrographic microscopy, geochemical techniques, and field study. It covers the mineralogy, chemistry, textures, and sedimentary structures that characterise sedimentary rocks, and relates these features to the depositional origin of the rocks and their subsequent alteration by. Strongly peraluminous granites (SPGs) form through the partial melting of metasedimentary rocks and therefore represent archives of the influence of assimilation of sedimentary rocks on the. The most common carbonate sedimentary rocks are limestone and dolostone, but also Sodium and Potassium Carbonates are common. Limestone is a sedimentary rock composed mainly of calcium carbonate (CaCO3), usually calcite, sometimes aragonite. As well it may contain considerable amounts of magnesium carbonate (dolomite).   If one compares the two classifications, a Rock rich in carbonate mud is termed a micrite by Folk and a mudstone or wackestone by Dunham. Moreover, a Rock containing little matrix is termed a sparite by Folk and a grainstone or packstone by Dunham.

In a lithic sandstone, the grains are mostly small rock fragments. A Wacke is a sandstone that contains more than 15% mud (silt and clay sized grains).. Sandstones are one of the most common types of sedimentary rocks. Mudrocks are made of fine grained clasts (silt and clay sized). Origin of carbonate sedimentary rocks (English) There is an Open Access version for this licensed article that can be read free of charge and without license restrictions. The content of the Open Access version may differ from that of the licensed version. Journals & Books; Help; The objective of this chapter is to evaluate some of the proposed classifications of sedimentary carbonate rocks, and to present suggestions for naming and describing them. It is not an historical review of existing schemes of classification alone, although a critical appraisal has been made of the various systems Cited by:   Noel James, Professor of Geology at Queen’s University, Canada, has, for over 40 years focused his research on carbonate sediments and rocks that range from the modern seafloor to the Archean, studying their origin via extensive marine and terrestrial fieldwork, petrography, and geochemistry. He has taught numerous courses on oceanography, carbonate sedimentology, Brand: Wiley.