上一条: 西天山高压脉及主 岩的氧同位素研究--古俯冲带深部流体及俯冲特征的启示
下一条: Unilateral Magma Emplacement of the Telimbela Batholith in the Central Ecuadorian Arc: Implications for Kinematics of Oblique Subduction of the Farallon-Nazca Plate