| 龙门山造山带岩石圈演化的动力学模式 |
| |
| 引用本文： | 罗志立.龙门山造山带岩石圈演化的动力学模式[J].成都理工大学学报(自然科学版),1991(1). |
| |
| 作者姓名： | 罗志立 |
| |
| 作者单位： | 成都地质学院石油地质勘查系 |
| |
| 摘 要： | 在对龙门山的构造变形、沉积环境、地层古生物、石油地质、遥感地质、地球物理、同位素地质等专题研究基础上,综合归纳出龙门山造山带岩石圈演化的动力学模式——为多层次、乡阶段、深层破裂控制浅层变形的陆内俯冲模式。它不同于A型俯冲带模式,也不同于阿尔卑斯碰撞型造山模式,而是具有中国特色的C型(中国型)俯冲造山模式。
|
| 关 键 词： | 龙门山造山带 动力学模式 陆内俯冲 A型俯冲 碰撞造山 C型俯冲 推覆构造 滑覆构造 |
THE DYNAMICAL MODEL OF THE LITHOSPHERIC EVOLUTION TN LONGMENSHAN OROGENIC BELT |
| |
| Luo Zhili.THE DYNAMICAL MODEL OF THE LITHOSPHERIC EVOLUTION TN LONGMENSHAN OROGENIC BELT[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1991(1). |
| |
| Authors: | Luo Zhili |
| |
| Abstract: | Depending on the studies of structural deformation, deposftional enviroments, stratigraphyand palaeontology, remote sensing geology, geophysics, petroleum geology and isotop geology, it ispointed out that the dynamical model of the lithospheric evolution in Logmenshan Orogenic Belt ismultilayered, multistaged and deep-fracture controlling shallow-deformation intracontinental subdu-ction medel, which is different not only from Ampferer-subduction model, but also from Alps-typedcollision orogenesis model, and which possesses the characteristics of Chinese-subduction model. |
| |
| Keywords: | Longmenshan Orogenic Belt dynamical model intracontinental subduction model Ampferer-subduction collision orogenesis Chinese-subduction nappe gliding nappe |
| 本文献已被 CNKI 等数据库收录！ |
|
