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Titlebook: Exposed Cross-Sections of the Continental Crust; Matthew H. Salisbury,David M. Fountain Book 1990 Kluwer Academic Publishers 1990 Deformat

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书目名称Exposed Cross-Sections of the Continental Crust
编辑Matthew H. Salisbury,David M. Fountain
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Exposed Cross-Sections of the Continental Crust;  Matthew H. Salisbury,David M. Fountain Book 1990 Kluwer Academic Publishers 1990 Deformat
描述In the Fall of 1988, 64 geologists and geophysicists from 11 countries met in Killarney, Ontario, on the north shore of Lake Huron to examine evidence that suggests that the continental crust is exposed in cross-section at several key locations on the Earth‘s surface. The meeting, which was held under NATO auspices as an Advanced Study Institute, was a landmark event in that it was the first time that many of the lead scientists working on these complexes in relative isolation around the world had‘ ever gathered together to compare results. The present volume is a compendium of the invited lectures given on the principle sections, plus an array of supporting papers on these and other sections as well as on related topics such as crustal emplacement mechanisms, deformation and rheology. Nearly all of the best known sections are represented, including the Ivrea Zone, Calabria, the Kapuskasing Zone, Fiordland and many others. It is our hope that this Volume will serve as a reference for Earth scientists who are trying to understand levels of the crust not normally exposed to view, as well as a point of departure for new research and a teaching aid to new entrants in this relatively ne
出版日期Book 1990
关键词Deformation; evolution; fault; uplift; structural geology
版次1
doihttps://doi.org/10.1007/978-94-009-0675-4
isbn_softcover978-94-010-6788-1
isbn_ebook978-94-009-0675-4Series ISSN 1389-2185
issn_series 1389-2185
copyrightKluwer Academic Publishers 1990
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发表于 2025-3-21 20:18:17 | 显示全部楼层
Exposed Cross-Sections of the Continental Crust978-94-009-0675-4Series ISSN 1389-2185
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Nato Science Series C:http://image.papertrans.cn/e/image/319757.jpg
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https://doi.org/10.1057/9781137317018ted seismic velocities have lead to the model of an exposed crustal section comprising the following units: 1) the Ivrea Zone with peridotites, mafic rocks and paragneisses in the amphibolite and granulite facies (lower crust and basal intermediate crust); 2) the Strona-Ceneri and Val Colla Zones wi
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https://doi.org/10.1007/978-981-10-3926-3 can trace a rock sequence from granulite-grade (from 7.5 to 5.5 kbar) through granitoids and amphibolite-facies gneisses into unmetamorphosed Paleozoic and younger sediments. The upper and the lower crustal sections are believed to have been part of the same crustal sequence since the late Hercynia
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The Political Academic: Dr. Walter Rodney,tion through a Tertiary extensional orogen in the eastern Great Basin, western U.S. Cordillera. Oligocene-Miocene sedimentary and volcanic rocks were deposited during brittle, upper-level crustal extension dominated by high-angle normal faults, rotation of the strata and the faults themselves, and t
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