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Ma, on amphibolite facies conditions, following the Triassic collision between the Sino Korean and Yangtze cratons.
残余的同碰撞及超高压构造只保留在较大的榴辉岩及其他超高压变质岩体内部。
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Secondary orthopyroxene has also been documented in mantle peridotite xenoliths derived from beneath both active arcs and ancient cratons.
交代的斜方辉石在现代活动岛弧和古克拉通的地幔橄榄岩捕掳体中多有报道。
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collision between the North China and Yangtze cratons.
这套岩石在印支期(约230 Ma)华北与扬子板块碰撞过程中经历了低温高压蓝片岩—榴辉岩相变质作用。
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Such cratons as Tarim and Yangtze are still of the thermal state for Precambrian lithosphere, while for North China craton, it is characteristiced by the thermal state for Mesozoic-Cenozoic lithosphere, due to reactivation associated with tectonic alternation.
中新生代期间西太平洋板块的俯冲和印度—欧亚大陆的碰撞等地球动力学过程分别控制了中国东、西部盆地的现代地温场特征。
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It is suggested that North China and Yangtze Cratons had ever been a unified craton, called Palaeosinica Craton, within which NNE-trending structural framwork was dominant, untill to the end of Palaeoproterozoic.
提出了 古元古代华北克拉通与扬子克拉通可能为一个统一的克拉通,暂称之为古中国克拉通,并且这一克拉通内的主导性构造线方位是NNE向。
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