来自西藏的热而干燥的深层地的石
1Geological Sciences, University of California, Santa Barbara, CA 93106, USA. Mineralogisch-Petrographisches Institut, University of Bern, Baltzerstrasse 1, CH-3012 Bern, Switzerland. Institut fur Geologie, Technische Universitat Bergakademie.
概括
在西藏高原的西藏高原.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 石化学 石化学是一门学科.
背景情况:
- 来自西藏中部高原的肖肖尼特岩含有异石.
- 这些石提供了对深层地条件的洞察.
研究的目的:
- 研究西藏高原中部地的热条件和融化过程.
- 为了确定是否发生广泛的地融化.
主要方法:
- 无水元沉积物和地质石的分析.
- 计算P波速度和波桑比率.
- 计算的地震特性与地震学观测结果的比较.
主要成果:
- 在30-50公里深处,石显示温度梯度为800-1000°C.
- 在提取前,石的加热达到200°C.
- 缺乏含水矿物质和地震数据与广泛的地融化相矛盾.
结论:
- 中部西藏地的温度足以使的脱水融化.
- 地震数据和矿物学数据表明地的广泛融化程度有限或不存在.
- 深层地的热制和融化过程是复杂的.
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