The alkine and K rich volcanic rocks, which are source rocks of zeolite ores, formed in middle late Yanshanian stage, with tectonic dynamic mechanism of compression and left lateral shearing.

  • 燕山中晚期以挤压-剪切(左行)为主的构造动力学机制控制了富碱高钾火山岩的发育,为沸石矿源岩的形成期;

  • 互联网摘选 2025-01-19 23:53:42

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