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- W1520551388 abstract "磷灰石分裂轨道(在船尾) 从 Xiaonanchuan 的七件样品的 thermochronology () 在 Kunlun 的 pluton () 通行证区域被执行，为决定预定冷却和在发掘和 morphotectonic 之间的关系的目的处理。在船尾，年龄产出 0.020 0.035 mm/a 的低剥光率在期间晚中新世，它对应于稳定的似地球形状、弱的构造高举环境。低剥光率能被看作近似的构造高举率。在船尾，地球年代学显示出阵发联盟者 rapid 自从上新世和在 Xiaonanchuan 区域超过 3 km 拆去的明显的材料，冷却。这不是简单剥光的结果。快速的冷却被结合集中的造山运动自从上新世，它被构造高举驾驶。加速的地势大楼被一系列指责伴随，它引起了盆和山谷形成并且下沉。AFT 年龄的空间模式也显示出微分高举，它减少向北方。这个趋势被支持由地区性在船尾数据，它显示发掘减少在东方 Kunlun 向北方。这个趋势也从西方的 Kunlun 范围在东方西方取向存在到东方。高举的趋势被似地球形状的特征也象迟了的新生代火山作用的分发一样包括举起和消除差别支持。给词调音：东方 Kunlun；西藏；Xiaonanchuan；磷灰石分裂轨道；morphotectonic；上新世" @default.
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- W1520551388 date "2006-01-01" @default.
- W1520551388 modified "2023-09-23" @default.
- W1520551388 title "Fission Track Geochronology of Xiaonanchuan Pluton and the Morphotectonic Evolution of Eastern Kunlun since Late Miocene" @default.
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