201831 · The two zones are a Triassic granite area and a middle Jurassic granite area, and the four belts consist of three compression-extensional volcano-intrusive rock belts, and an extensional volcano-intrusive rock belt.
view more2012101 · Whole-rock major and trace elements Thirty-six samples were analyzed for major and trace element compositions, including eight samples from Maotan granite and Huayuangong granite each, ten samples from Xiangshuijian granite and Banshiling granite each. The major and trace element data are summarized in Tables 1 and A.1.
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view more201817 · Abstract Magma mixing commonly takes place between isotopically depleted mafic and enriched felsic magmas. Here we present isotopic evidence exhibiting the opposite behavior in the Early Cretaceous Siling complex (south China), which is composed of gabbro, quartz diorite, granodiorite, and alkali feldspar granite with locally many mafic …
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view more2012101 · Highlights A 1 granite forms in intraplate settings, whereas A 2 granite forms at convergent margins. A-type granites in central eastern China are classified into A 1 and A 2 chemical subgroups. Spreading ridge is a major component of the mega engine that initiates and drives plate tectonics. Ridge subduction may results in both A 1 and A 2 …
view more20231216 · This belt can be segmented into four tectonic units: the northern margin of the South China Block, South Qinling Belt, North Qinling Belt and the southern margin of the North China Block from ...
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view more2021331 · The narrow greenstone belts that separate the granite domes of the Pilbara are remnants of cold, dense, hydrated mafic crust, up to 20-km thick, which sank between buoyant and rheologically weak ...
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