问题描述：
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?
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?
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