英文导游词翻译Sanqing Mountain is located at the conjunction between the Yangtze Plate and the Huaxia plate, north to it is the Jiangxi Northeast suture cincture deep fault. Ever since the Indochina movement, Sanqing has entered continent marg

英文导游词翻译Sanqing Mountain is located at the conjunction between the Yangtze Plate and the Huaxia plate, north to it is the Jiangxi Northeast suture cincture deep fault. Ever since the Indochina movement, Sanqing has entered continent marg
英文导游词翻译
Sanqing Mountain is located at the conjunction between the Yangtze Plate and the Huaxia plate, north to it is the Jiangxi Northeast suture cincture deep fault. Ever since the Indochina movement, Sanqing has entered continent margin violent changes and Pro-Pacific Ocean structure development stage. At late Yanshan movement period, a large scale of acid magma intrude activities took place under the integrative effect of three faults in Northeast-East, North-Northeast and North-West. Sanqing were uplifted during (at) late Himalayan period. The sediment of Carbonate which deposited during the Carnbrian and Ordovician even late C, P and early Triassic was eroded more easily than the harder granite. The granite rocks were exposed as a result the granite mountains further developed their characteristic shape through erosion and dissection. Sanqing continues to be uplifted till now. 这段英文的中文是什么?

英文导游词翻译Sanqing Mountain is located at the conjunction between the Yangtze Plate and the Huaxia plate, north to it is the Jiangxi Northeast suture cincture deep fault. Ever since the Indochina movement, Sanqing has entered continent marg
三清山位于之间的结合扬子板块与华夏板块,北部是江西东北部缝合带深大断裂.自印度支那运动,三庆已进入大陆边缘暴力的变化和临太平洋结构的发展阶段.在晚燕山运动时期,大规模的酸性岩浆侵入活动发生的综合效应的三个断层在东北地区,东北和西北.三庆被抬升过程中（在）晚喜马拉雅期.在碳酸盐沉积物的沉积在Carnbrian和奥陶纪后期甚至ç ,磷,早三叠世被侵蚀更容易就越难花岗岩.花岗岩岩石暴露,由于山区的花岗岩进一步发展其形状特征通过侵蚀和剥离.三庆继续抬升到现在.

Sanqing山位于契合在扬子板材和华夏板材之间，北部对它是江西东北缝合带深刻的缺点。 自印度支那运动， Sanqing输入大陆边际猛烈变动和赞成和平的海洋结构发展阶段。 在晚Yanshan运动期间，大规模酸岩浆在东北部东部，北部东北部闯入活动发生了在三个缺点之下的综合作用和西北部。 Sanqing是上升的在(在)晚喜马拉雅期间。 放置在Carnbrian期间，并且奥陶纪晚C，甚而P和早Trias...

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Sanqing山位于契合在扬子板材和华夏板材之间，北部对它是江西东北缝合带深刻的缺点。 自印度支那运动， Sanqing输入大陆边际猛烈变动和赞成和平的海洋结构发展阶段。 在晚Yanshan运动期间，大规模酸岩浆在东北部东部，北部东北部闯入活动发生了在三个缺点之下的综合作用和西北部。 Sanqing是上升的在(在)晚喜马拉雅期间。 放置在Carnbrian期间，并且奥陶纪晚C，甚而P和早Triassic比更加坚硬的花岗岩更加容易地被腐蚀碳酸盐的沉积。 结果花岗岩岩石被暴露了花岗岩山通过侵蚀和解剖进一步开发了他们的典型形状。 Sanqing继续是上升的直到现在。

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