盆山转换时期所形成的变质流体为多相盐水流体，形成于变形的初期。
The studies indicate that the fluid formed during the basin mountain transition is metamorphic fluid with multi phase salt water formed in the initial stage of deformation.
从而为正确认识古特提斯洋的演化和盆山转换过程提供了强有力的地球化学证据。
This provides strong geochemical evidences for correctly understanding the evolution of the old Tethys and the basin range transition.
因此，盆山转换研究、探索盆转山和山控盆的过程则成为大陆地质的前沿研究领域。
The researches on the basin range transition thus become the frontiers of continental geology.
应用推荐