认为区内早埃姆斯期属深水陆棚至深水盆地沉积环境，为龙门山区泥盆纪沉积盆地的性质和演化提供了新资料。
This new explanation has provided new evidences for the interpretation of the nature and evolution of the Devonian sedimentary basins in the Longmen Mountain area.
与粘土化有关的流体为流体演化的晚期产物，属低温、低盐度流体。
The fluids related to argillation formed in late evolution stage and is of lower temperature and lower salinity.
本文中还讨论了蕺菜属植物的起源演化。
In this article the origination and evolution of genera Houttuynia cordate is discussed as well.
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