Received date: 1994-03-21
Online published: 1994-11-01
Cherts are widely distributed on the surface of the earth and are a special type of sedimentary rocks. On one hand, they retain abundant and reliable information of palaeogeography, palaeoclimate and palaeoenvironments because of their high hardness and strong resistance to weathering; on the other hand, they are closely related to organism evolution an formation of some sedimentary ore deposits. Those two aspects make it become one of the hot research projects in the cycle of sedimentology with very important theoretical and practical significance. On the basis of the imformation from a wide variety of retrieval tool books and published literatures, the author has summarized the history of chert research abroad and discussed its present state of art and future developing trends. By comparison of chert research in China, several suggestions have been made to change the under developed state in this field.
Key words: Chert; Research progress.
Tang Shirong,Wang Dong’an . ADVANCES IN CHERT RESEARCH[J]. Advances in Earth Science, 1994 , 9(6) : 71 -75 . DOI: 10.11867/j.issn.1001-8166.1994.06.0071
[1] 王东安.扬子地台晚元古代以来硅岩地球化学特征及其成因.地质科学,1994,29(1):41-54.
[2] 丁悌平等.硅同位素测量方法研究.见:称定同位素分析方法研究进展,地质矿产部矿产地质研究所同位素地质研究室编,北京:科学技术出版社,1992.1-8.
[3] Asdton S R (ed.) Silicon Gechemistry and Biogeochemistry. Academic Press,Lodon,1983.
[4] Eley B E. Cherts of Southern Onrario.Toronto: Royal Ontario Museum, 1989.
[5] Hein J R (ed.) Siliceous Sedimentary Rock-hosted Ores and Petroleum. Van Notrand Reimhold Company, New York, 1987.
[6] Hein J R et al.(ed.) Siliceous Deposit of the Tethys and Pacific Regions.Springer-Verlag,Heidelberg,1989.
[7] Iijima A et al.(ed.) Siliceous Deposits in the Pacific Regions.Elsevier, NewYork,1983.
[8] Ireland H A (ed.) Silica in Sediments. SEPM Special Publication No.7. Tulsa, Oklahoma, 1956.
[9] MacBridge E F (ed.) Silica in Sediments: Nodular and Bedded Chert. SEPM Reprint Series Numbers, Tusla, Oklahoma,USA,1979.
[10] Matheney R K and Kmauth L P.New isotopic temperature estimates for early silica diagenesis in bedded cherts. Geology (Boulder), 1993, 21(6):519-522.
[11] Jafri S H, Balaram V and Govil P K. Depositional environments of cretaceous radiolarian cherts from Andaman-Nicobar islands, Northeastern Indian Ocean. Maine Geology,1993,112(1/4):291-301.
[12] Winter B L and Knauth L P. Stable isotope geochemistry of cherts and carbon are from the 2.0 Ga Gunflint Iron Fomation: Implications for the depositional setting for the effects of diagenesis and metamorphism.Precambrian Resarch, 1992, 59(3/4):283-313.
[13] Murry R W. Indentifying depositional environments of chert usingchemical techniques: an overview of general principles and a synthesis of 45 published results (abstr.). Geological Society of America, 1993, Abstracts with Programs. 1992,24(7):213.
[14] Hagddtrum J T and Murry B L.Deposition of Fransican Complex cherts along the Paleoquater and accretion to the Ametican margin at tropical paleolatitudes. Geological Society of American Bulletin,1993,105(6):766-788.
/
〈 |
|
〉 |