西湖凹陷 meaning in Chinese
xihu trough
Examples
- It is a late cretaceous to tertiary basin located on the eastern part of the continental shelf of the east china sea ; it occupies an area of 59 , 000 km2
西湖凹陷是晚白垩第三纪盆地，位于中国东海大陆架的东部，面积590000km2 ，处于纬度124030 '与127000 '之间，经度28030 '与31000 '之间。 - It is bounded by longitude of 124o30 " to 127o00 " and latitude of 28o30 " to 31o00 . having known the geologic and tectonic background of xihu depression , to evaluate the play , to reconstruct the burial history of the basin and build thermal and
了解西湖凹陷的地质与构造背景之后，依次进行系列研究：重建盆地的埋藏史、热史与成熟史模型，以及相继划分可能的含油气系统。 - To sum up the above analysis , we make sure that the pretertiary of haijiao uplift , yushan uplift and east flank in oujiang depression and the transitional zone between changjiang depression and xihu depression is a new prospect of time and space for hydrocarbon exploration in the shelf basin of the east china sea
因此，海礁凸起、渔山凸起、瓯江凹陷东侧、长江凹陷与西湖凹陷之间以及浙闽隆褶带的前第三系是东海陆架区油气勘探的新领域。 - During late mesozoic and cenozoic , extensions were widespread in eastern china and adjacent areas . the induced compressions and extensions , uplifting and subsidence as well as large - scale magamatism , increased the pre - existing ne - nne trending faults , uplifts and subsidence belts . this is how ; the giant transform structure led to the formation of xihu depression
在晚中生代与新生代，拉张作用广泛分布于中国东部及邻区，导致了挤压与拉张、隆起与沉降以及大规模的岩浆作用，于是使早先存在的北东北北东向断层、隆起带与沉降带增强，这也是大的转换断层形成西湖凹陷地层的机理。