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- W2387699170 abstract "A study of structures, deformation and strain of country rocks around Fangshan pluton in the western Hills, Beijing, reveals a high-temperature shear aureole, domal distribution of steep lineations and foliations in the thermodynamic aureole, and ring synclines around the pluton. Combining with the analysis of the regional tectonic events, it is concluded that Fangshan pluton is a real magmatic diapir (hot-stokes diapir). To our knowledge, this is the first reported magmatic diapir in the world. As such, this research result argues for a reconsideration of the structural frame and deformational series of the Zhoukoudian area. It is suggested that the Fangshan metamorphic core complex did not exist; the Guandi Archean complex in the margins of the pluton was outcropped by ductile flow of the diapiric ascent; previously proposed Indosinian denudational faults were piercing structures and/or the absence of the strata in the high temperature shear aureole; Taipingshan and Fenghuangshan synclines are ring synclines around the pluton formed by drag of country rocks due to the diapiric ascent." @default.
- W2387699170 created "2016-06-24" @default.
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- W2387699170 date "2005-01-01" @default.
- W2387699170 modified "2023-09-25" @default.
- W2387699170 title "Magmatic Diapir of Fangshan Pluton in the Western Hills, Beijing and Its Geological Significance" @default.
- W2387699170 hasPublicationYear "2005" @default.
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