
 The intrusive rocks in the Tarim LIP, mostly exposed at Xiaohaizi and Wajilitagof the Bachu area (Fig. 3.1), include ultramafic–mafic layered intrusions, syeniticrock bodies (and perhaps some A-type granitic plutons), radiating mafic dikeswarms, and ultra (共 1490 字) [阅读本文] >>


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