机译:分层式对流岩石圈下沉继续科罗拉多高原的隆升
Earth Science Department, Rice University, Houston, Texas 77005-1892, USA;
Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA;
Department of Earth Sciences,University of Southern California, Los Angeles, California 90089-0740, USA;
Earth Science Department, Rice University, Houston, Texas 77005-1892, USA;
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA;
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA;
Earth Science Department, Rice University, Houston, Texas 77005-1892, USA;
Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA;
机译:岩石圈密度模型揭示了低地壳水化作用对科罗拉多高原和大平原新生代隆升的证据
机译:科罗拉多高原隆起的岩石圈局部分层模型的地震证据
机译:科罗拉多高原与大盆地对比的岩石圈结构-科罗拉多高原-大盆地被动实验的初步结果。
机译:藏高原中生代和新生代火山主义的景观和地球化学变化及其对高原岩石术进化的动态推断
机译:使用瑞利波层析成像技术对科罗拉多高原及其附近地区的岩石圈结构进行成像。
机译:法拉隆俯冲板在科罗拉多高原下的次大陆岩石圈地幔的灾难性剪切作用
机译:熔融平衡深度作为欧亚 - 阿拉伯碰撞期间岩石厚度的传感器和Anatolian高原的隆起