Geological Structure and Geodynamical Development of Kazakhstan Territory

摘要：

　　According to the seismic tomography, the lithosphere formation of Kazakhstan has a plume origin.Kazakhstan in the Paleozoic was a separate continent and consisted of three concentric rings of bounded geometry sutures.The rings under the active influence of mantle plume made vertical movement and their axes made horizontal movement.The development of variously oriented lineaments led to the formation of clumpy-block structure.The modern structure of Kazakhstan was formed during the interaction with Europe, Siberia and southern continents during the Paleozoic-Cenozoic.

关键词： Kazakhstan the crust deep structure continents and oceans mantle plumes ring structures geological formations

作者: Adilkhan Baibatsha

作者单位: Geology department Kazakh National Research Technical University named after K.I.Satpayev KazNRTU Almaty, Kazakhstan

会议类型: 国际会议

会议名称: The 7th International Conference on Environmental and Engineering Geophysics & Summit Forum of Chinese Academy of Engineering on Engineering Science and Technology (ICEEG 2016)(第七届环境与工程地球物理学国际会议)

会议地点: 北京

会议语种:英文

页码: 432-435

在线出版日期: 2016-06-27（万方平台首次上网日期，不代表论文的发表时间）