The nature of the lithosphere-asthenosphere boundary (LAB)

摘要：

The bottom of the seismic low-velocity zone (LVZ) beneath the ocean basins is at about 220 km depth,whereas the top is determined by the thickness of the lithospheric lid. Conductive heat loss or thermal contractioncan explain both the ocean depth (first order) and lithosphere thickness (L) as a function oflithosphere age (i.e., L/Age, or the half-space model (HSM》.

作者: 牛耀龄

作者单位: School of Earth Science, Lanzhou University Department of Earth Sciences, Durham University

会议类型: 国内会议

会议名称: 2011年全国岩石学与地球动力学研讨会

会议地点: 西安

会议语种:英文

页码: 173-174

在线出版日期: 1900-01-01（万方平台首次上网日期，不代表论文的发表时间）