共查询到20条相似文献,搜索用时 15 毫秒
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J. H. McBride A. J. M. Pugin W. J. Nelson T. H. Larson S. L. Sargent J. A. Devera F. B. Denny E. W. Woolery 《Tectonophysics》2004,383(3-4):243-244
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Luca Caracciolo Salvatore Critelli Fabrizio Innocenti Niko Kolios Piero Manetti 《Sedimentology》2013,60(3):865-869
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EMILIANO MUTTI DANIEL BERNOULLI FRANCO RICCI LUCCHI ROBERTO TINTERRI 《Sedimentology》2010,57(3):933-934
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M.R. St-Onge 《Tectonophysics》1981,76(3-4)
Three progressive metamorphic suites are developed in pelitic rocks of the northern Wopmay Orogen. Two suites are related to the Hepburn Batholith and one to the Wentzel Batholith. All three suites are cut by post-metamorphic wrench faults, some of which have significant vertical displacement. The structural relief so provided reveals that medium-and high-grade isograds associated with the Hepburn Batholith dip inward towards the batholith and are thus “hot-side-up”. Isograds associated with the Wentzel Batholith dip away from the batholith and are thus “hot-side-down”. It is concluded that Hepburn Batholith has the form of the flattened funnel fed from depth, and that Wentzel Batholith is the arched roof of an intrusive complex of unknown shape at depth. 相似文献
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K.C. Gyani 《Gondwana Research》1998,1(3-4):431-432