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The Origin of Spots in contact aureoles and Over-Heating of Country Rock Next to a Dyke

Journal of Earth Science 2018年第5期29卷 1005-1009页

作者： Roger Mason Rong Liu School of Earth Sciences China University of Geosciences

Petrographic comparison of andalusite in the contact aureole of the Fangshan pluton, Zhoukoudian, Beijing, China, and hornfels in the aureole of the Markfield diorite, Leicestershire, Eng- land, shows that spots characteristic of the outer zones of contact metamorphic aureoles did not form during the progressive stage of contact metamorphism, but are pseudomorphs after earlier andalusite with characteristic chiastolite microstructure. The baked margin produced by contact metamorphism of syenite against a dyke in the Houshihushan ring complex, Shanhaiguan, Hebei Province, China, is an unusual feature caused by the dyke＇s role as a feeder to a family of cone-sheets.

关键词： contact metamorphism contact aureole retrogression hornfels spots Zhoukoudian Houshihushan.

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Melting of carbonate wall rocks and formation of the heterogeneous aureole of the Panzhihua intrusion,China

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Geoscience Frontiers 2013年第5期4卷 535-546页

作者： Clement Ganino Nicholas T.Arndt Catherine Chauvel Alexandre Jean Charlotte Athurion Geoazur Universite de Nice-Sophia AntipolisCNRS/IRD250 rue Albert Einstein06560 ValbonneFrance ISTerre Grenoble UniversitesCNRS/IRDBP 5338041 GrenobleCedex 9France

The Panzhihua gabbroic intrusion,part of the plumbing system of the Emeishan large igneous province, intruded late-Proterozoic dolomites and marls about～263 Ma *** dolomites in the contact aureole were converted to brucite marbles and a diverse suite of forsterite,diopside and garnet *** variation in mineralogy is explained in part by differences in the composition of the protolith,particularly the proportion of silica minerals and clay,and in part by transfer of elements from intruding *** trace element compositions of most marbles and skarns are very similar to those of unmetamorphosed dolomites and marls,but some contain high Si,Ti,and Fe contents that are interpreted to have come from a magmatic *** brucite marbles sampled～10 m from the contact of the intrusion and named ＂enriched brucite marble＂ have trace element compositions very different from their dolomitic protolith：their rare earth elements are strongly enriched whereas levels of Nb-Ta,Zr-Hf and Ti are very *** characteristics resemble those of carbonate liquid in equilibrium with silicate liquid or more probably with silicate minerals in the case of Panzhihua,a similarity we take to indicate that the sample underwent partial *** taken up to 300 m from the contact contain brucite indicating that high temperatures persisted well into the country ***,other samples collected only tens of metres from the contact are only slightly recrystallized indicating that conditions in the aureole were highly *** suggest that temperatures within the aureole were controlled by conduction of heat from the main intrusion and by supply of additional heat from abundant small dykes within the *** of fluids derived from deeper levels in the aureole flushed the carbon dioxide from the dolomite,lowering temperature needed to partially melt carbonate to the temperatures attained near the *** but extensive heating destabilized the carbon

关键词： Panzhihua Melting Carbonates contact aureole Thermal metamorphism Petrology

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