钴（金）矿石组构及矿石矿物的世代显示其主要与海底喷气沉积成矿作用有关，在后期的碰撞造山过程中，受到了改造和活化。
The ore structure and generation of cobalt-gold ore minerals suggest that their formation mainly related to submarine sedimentary exhalation, reformed and mobilized in late collision orogenesis.
通过计算绝热压缩温升和畸变形能沉积产生的温升，给出熔化判据，定量估计出了在小碰撞角下爆炸焊接界面熔化层厚度。
Throughcalculation of temperature rising callused by them, melt criterion is given, the thickness of melted layer near explosive welding interface with small collision Angle is estimated.
东昆仑造山带具有软碰撞、多旋回的特点，造山带内的沉积盆地具有多物源和不同的大地构造背景。
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles. The sedimentary basins inside it have multi-sources and different tectonic backgrounds.
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