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Titlebook: Basement Tectonics 13; Proceedings of the T A. Krishna Sinha Conference proceedings 1999 Kluwer Academic Publishers 1999 Cambrian.Petrogene

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發(fā)表于 2025-3-21 19:52:07 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Basement Tectonics 13
期刊簡(jiǎn)稱Proceedings of the T
影響因子2023A. Krishna Sinha
視頻videohttp://file.papertrans.cn/181/180937/180937.mp4
學(xué)科分類Proceedings of the International Conferences on Basement Tectonics
圖書(shū)封面Titlebook: Basement Tectonics 13; Proceedings of the T A. Krishna Sinha Conference proceedings 1999 Kluwer Academic Publishers 1999 Cambrian.Petrogene
影響因子The Thirteenth International Conference on Basement Tectonics was held on the campus of Virginia Polytechnic Institute and State University in Blacksburg, Virginia from June 2 -6, 1997. The oral presentations and discussions over three days covered a wide range of topics, and provided the international audience with a perspective on scientific efforts underway around the world. The conference participants were able to attend two separate field trips: (I) a pre-conference trip guided by Professor Robert Hatcher of the University of Tennessee, Knoxville, examined the Basement rocks in the North Carolina -Tennessee region of the Appalachian Mountains, and (2) a mid-conference field trip guided by A.K. Sinha, convener of the conference, allowed participants to examine the complex rock associations and structures of the> 1000 m.y. old basement rocks in Virginia. Both the field trip guidebooks and abstract volumes were published for the conference. The meeting brought together scientists from more than 14 countries. Their participation, and the fiscal success of the meeting would not have been possible without the support of the Department of Geological Sciences, the College of Arts and
Pindex Conference proceedings 1999
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New Data and Interpretations for the Precambrian, Midcontinent USA Midcontinent USA. Petrographie analysis has been done for samples from wells penetrating the Precambrian surface. Chemical analysis is available for rock types such as rift basalt, carbonatites, arch metamorphic and granitic plutons. A few isotopic ages are available to weave together the physical
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Zircon Ages of Basement Orthogneisses from the Northern Segment of the Araguaia Belt, Brazilnt orthogneisses that occur in the core of several dome like structures in the northern segment of the Araguaia belt, Brazil. These studies were carried out to understand the stratigraphic relationship among the different gneisses, and to constrain interpretations concerning the age of the structura
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