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Updated: Jul 20, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
西藏高原的斜坡逐步上升和增长
P Tapponnier1, X Zhiqin, F Roger
1Institut de Physique du Globe, 4 Place Jussieu, 75252 Paris, France. tappon@ipgp.jussieu.fr
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
- 板块构造学是一种板块构造学.
- 地力学是什么?地力学是什么?
背景情况:
- 两种模型解释了西藏的高海拔:广泛的地流或石灰岩层块之间的局部剪切.
- 最近的代变形,岩石和地震数据支持局部剪切模型.
研究的目的:
- 为了研究高藏高原的形成机制.
- 分析中生代变形,岩石运动和地震结构.
主要方法:
- 考古变形模式的分析.
- 检查岩带及其年龄的进展.
- 解释地震结构. 地震结构的解释.
- 对地加厚和地幔脱的建模.
主要成果:
- 西藏高原的起发生在三个阶段,涉及陆地层推力的连续提升.
- 地的加厚伴随着地幔脱,而不是均的加厚.
- 在山间盆地的沉积在每一个升起阶段后都会形成平坦的高原.
- 北向年轻化的岩带表明亚洲地幔在北方范围以下的连续沉降.
- 斜俯冲和冲滑断层导致东部和东北地区的高原生长.
结论:
- 西藏高原的形成最好通过依赖时间的,石灰岩层块之间的局部剪切来解释,而不是统一的粘性流.
- 板块构造学,包括斜俯冲和滑坡划分,在高原的发展中发挥了重要作用,特别是它向东和东北扩张.
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