海西-印支期，华南地质构造发展进入新的阶段。
The geologic history of the South China developed into a new stage in the Hercynian - Indochina period.
岩体以小岩株、岩脉及构造岩片产出，普遍受后期构造作用，多数以构造片岩卷入海西期苦海-赛什塘构造混杂岩带内。
The intrusive bodies are output in stocks, dikes and tectonic slices, which were suffered from later tectonism and evolved in the Kuhai-Saishitang Hercynian mélange belt as tectonic slices.
其成因主要为燕山和海西期的构造运动下形成的。
Origin cause of formation its form under the tectonic movement, the west of issue for swallow mountain and sea mainly.
埕岛油田位于渤海西南部极浅—浅海地区，是一个大型潜山披覆构造油田。
Chengdao oilfield, located in an extremely shallow-shallow offshore area of the southwestern Bohai, is a large drape structure over buried hills.
矿床在海西早期的构造动力条件与整个闽西南区域性的主体构造动力条件不同，并且经历过明显的同沉积构造变动。
The tectonic dynamic condition of Makeng, which is different from the regional tectonic dynamic condition of southwestern Fujian, experienced an alternation with an obvious syndepositional structure.
在琼库恰克构造带的形成和发展过程中经历了海西运动期古构造形成阶段及喜马拉雅运动期现今构造定型阶段。
The formation and development of Qongkuqak structural zone underwent two stages, i. e. , Hercynian paleostructural forming stage and Himalayan present-structural forming stage.
龙洞湾多金属矿床大地构造处于昆仑秦岭褶皱区秦岭褶皱系礼县-柞水-海西地槽褶皱带中部。
The Longdongwan polymetallic ore deposit geostructure is in middle the Kunlun Mountains Qinling folded region Qinling system of fold Li xian-Zashui Haixi geosyncline belt of folded strata.
以构造动力成矿系统理论为基础，通过构造成因及演化过程说明海西-燕山期是充水裂隙形成的重要阶段；
The structural information and evolution of the fissured-water pour-in on the basis of theory about Zhaoping structure mineralized dynamic system are analyzed.
海西-印支期，华南地质构造发展进入新的阶段。
The geologic of the South China developed into one new stage in the Hercynian-Indochina period.
临清坳陷白海西期以来各地质时期的盆地格局在垂向和横向上均存在着明显的差异，后期盆地对先期盆地进行了强烈的叠加构造。
Since Hercynian Era there have been obvious differences in vertical and horizontal basin pattern of Linqing depression, a strong superposition structure of post basin being on the earlier basins.
临清坳陷白海西期以来各地质时期的盆地格局在垂向和横向上均存在着明显的差异，后期盆地对先期盆地进行了强烈的叠加构造。
Since Hercynian Era there have been obvious differences in vertical and horizontal basin pattern of Linqing depression, a strong superposition structure of post basin being on the earlier basins.
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