| 三江褶皱系西南部的华力西运动 |
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| 引用本文： | 熊家镛. 1984. 三江褶皱系西南部的华力西运动. 地质通报,(2): 9-16. |
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| 作者姓名： | 熊家镛 |
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| 作者单位： | 云南省地质局区调队 |
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| 摘 要： | 本文重点讨论云南西南部景东—思茅—勐腊—线以西、澜沧江深断裂以东、景东以南区域华力西运动的性质、强度及其代表性。这一范围在大地构造上属三江褶皱系西南部,有人将其进一步划属兰坪—思茅坳陷,或称之为临沧一景洪褶皱带,但均强调该区印支运动的重要性,并认为是其主褶皱幕。
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THE VARISCAN MOVEMENT IN THE SOUTHWESTERN PART OF THE SANJIANG FOLD SYSTEM |
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| XIONG Jia-yong. 1984. THE VARISCAN MOVEMENT IN THE SOUTHWESTERN PART OF THE SANJIANG FOLD SYSTEM. Geological Bulletin of China,(2): 9-16. |
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| Authors: | XIONG Jia-yong |
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| Affiliation: | Regional Geological Survey Brigade,Geological Bureau of Yunnan |
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| Abstract: | From the data obtained in regional geological surveys in recent years this paper demonstrates that the area west of the line of Jingdong-Simao-Mengla,east of the Lanchengjiang deep fracture and south of Jingdong in southwest Yunnan is a Variscan fold belt. The late Paleozoic sediments in the area consist mainly of a considerable thickness（＞9500m） of volcanic-clastic rock formations,and there also occurs a spilite-keratophyre-radiolarian chert formation up to 1000 in in thickness,which undoubtedly implies a eugeosynclinal environment. In the entire Variscan cycle there existed two strong foldings; one took place between the Middle and Late Carboniferous,and the other at the end of the Late Permian. They both generated regional deformations and distinct angular unconformities,and were accompanied by relatively strong magmatism and metamorphism. The late Variscan movement is the principal folding episode that caused the Variscan geosyncline in the area to close and transform from the geosyncline stage to the platform stage. the overlying Triassic strata and those above them all possess the features of cover rocks. Therefore ihe principal cycle in the area should be the Variscan cycle,and this area should represent a Variscan fold belt. |
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