进一步分析，这些沉降中心的形成明显受到了周缘山系逆冲推覆作用的构造负载和盆地基底构造的制约，使盆地形成了隆坳相间的古地貌格局。
The formation of these quick subsidence centers were obviously controlled by the tectonic load derived from the adjacent orogenic thrusting and preexisting tectonic blocks in the basin basement.
礁分布可能受隐伏基底断裂活动所形成的古构造控制。
Reef distribution may be controlled by the paleostructure produced by the activities of buried basement faults.
盆地基底古热流是实现盆地地热场模拟的基础边界参数条件。
Basin basement palaeo-heat flow is a basic boundary parameter condition to realize basin geothermal field simulation.
应用推荐