三岩
- 网络Sangam;Saniwa
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其中,第二、三岩浆活动阶段分别早于燕山造山带在中、晚侏罗世末的两次主造山幕发生的时代,所以燕山地区主造山幕的P-T-t演化为逆时针轨迹。
The second and third stages of magmatism occurred before the main orogenic episodes in the end of mid-Jurassic and late-Jurassic , respectively ; therefore , the main orogenic episodes have counterclockwise ( CCW ) P-T-t path .
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文章运用人类学田野及跨文化比较方法,探讨三岩地区实行树葬的实际情况。
This article , by adopting anthropological fieldwork and cultural comparative studies , explores the detail of tree burial in Sanyan District .
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在狼山群第三岩组中发育韧性剪切带、棱岩、层掩卧褶铍及石香肠构造。
The ductile shear zone , mylonite , layer parallel lying fold and boudinage come out extensively in the third group of Langshan .
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同时,定义了三岩造林困难地,提出了三岩造林困难地的生态环境特点。
The difficult afforestation land of shale , limestone and calcium shale were defined and the ecological environment characteristics of that was pointed out .
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根据不同成岩成矿系列的时空分布,讨论了横断山地区三岩带的成岩成矿机理。
In conjunction with the temporal and spacial distributions of different petrogeno-minerogenetic series the mechanism of the Ailaoshan-Jinshajing magmatic complex belt is discussed as well .