| 青藏高原亚东—格尔木一带的活动构造及其与经济建设的关系 |
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| 引用本文：韩同林,郑英龙,唐哲明.1990.青藏高原亚东—格尔木一带的活动构造及其与经济建设的关系[J].地球学报,11(2):129-138. |
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| 中文摘要:亚东—格尔木一带的活动构造，以亚东-羊八井-温泉活动构造带、和属于一些边界翘起带和断块翘起带的一部分最为明显。地震活动主要与活动构造带中的断裂带有关，在进行有关工程建设时应尽量避开或采取必要的防震措施。地热活动主要受活动构造带中的断陷带制约，地热资源的寻找和开发利用应在现今活动构造表现强烈地段和南北向张性断陷带中及构造转折部位。水力资源主要分布于受活动构造强烈隆升作用形成的峡谷地段。 |
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| THE ACTIVE TECTONTICS ALONG YADONG—GOLMUD，QINGHA—XIZANG PLATEAU AND ITS RELATIONSHIP TO SOCIAL CONSTRUCTIONS |
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| Abstract:The active tectonics along Yadang—Golmud, Qinghai-Xizang Plateau mainly refer to Yadong-Yangbajing-Wenquan active tectonic belts, the Himalayan border tilting belts, the Gangdise fault block tilting belts and part of the eastern Kunlun boundary tilting belts. Earthquakes are closely related to the marginal faults of the active tectonic belts, so the seismic belts are consistent with the active tectonic belts. The structures controlling earthquakes are active tectonic bels, and the seismic, structures are boundary fracture belts. Geothermal activity is mainly controlled by the faulting depression zone belt in the arive tectonic belts. The intensity of the geothermal activity is mainly concerned to the intensity of the active tectonics, the mechanic nature of the faulting depression zones and its location in the tectonics. Hydropower resource is mainly controlled by the uplifting of the active tectonics, so the engineering and construction in this area should keep away from the boundary fracture belts or take needed precautions against earthquakes. Geothermal resources may be found and utilized in the north-south faulting depression zone where the active tectonics are intensive nowadays and at the bending or cross-cut parts of tectonics. Hydropower resources are richest at the gorges formed at the intersecting parts of north-south directional active tectonic belts and the Yarlungzangbo River bed. |
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