The Early Mesozoic magmatite developed on the tensional background caused by closing of Mongolia-Ehucike Residual Ocean in scissors form.The Later Mesozoic magmatite formed in compression background.
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- 中生代早期岩浆岩形成于蒙古-鄂霍茨克残余洋“剪刀式”闭合所造成的张性似裂谷环境,中生代晚期岩浆岩形成于挤压环境。