This theory could not explain the composition, structure and evolution of continental lithosphere and continental orogenic belt, and also is not in line with modern scientific theory.
上述理论阐明不了大陆岩石圈、大陆造山带的组成，结构与演化，也与当代的基础理论不尽吻合。
The formation and evolution of continental lithosphere has been one of important research projects in earth science field for these years.
绪论大陆岩石圈的形成与演化是近年来地球科学领域重要的前沿研究课题之一。
The topic of the study of the evolution of early crust is to probe into the processes of early continental formation, growth, and recycling, and their geochemical and geophysical models.
地壳早期演化研究的主题是探讨早期大陆形成、生长和再循环的地质过程及其地球化学和地球物理模式。
The regional tectonic evolution and extensive mineralization in orogenic belts are different expressions of the same continental dynamic process.
造山带区域构造演化与大规模成矿作用是同一大陆动力学过程的不同表现。
These transform fault series play an important role in the formation and the geological evolution of the Southeastern China continental margin basins and the tectonic-structural zones.
这些转换断层系统对中国大陆东、南缘含油气盆地和边缘构造带的形成和地质演化起着重要的作用。
Tectono -sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、弧后裂谷和拗陷盆地。
Tectono - sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、后裂谷和拗陷盆地。
Based on the analysis of the structure and the brief evolution history of the passive continental margin in West Africa, the dynamic background of formation and evolution of the margin is discussed.
通过对西非被动大陆边缘结构、构造特征，以及边缘发育演化简史的分析，探讨了西非被动大陆边缘形成演化的动力学背景。
The Okinawa Trough (OT) is the solitary active backarc basin in the world that is formed by extensional rifting in the continental marginal zone and is in the early stage of evolution.
冲绳海槽是当今世界上唯一的在大陆边缘张裂形成的、处于早期演化阶段的活动性大陆边缘弧后盆地。
The evolution of the fossil continental plate in China had been carried out under the general framework of global plate movement, thus it had been controlled by the global plate movement.
中国大陆古板块演化是在全球板块运动的总体框架下进行的，受全球板块运动的控制。
The present paper deals with the basic characteristics of the structures and their control and effect on the formation and evolution of the Mesozoic red continental basin in this area.
叙述了该地区推覆构造的基本特征及其对中生代陆相红盆的形成、演化过程的控制和改造。
Therefore they are corresponding to the three different featured convergent stages of ocean subduction, continental collision and intra-continent contraction in the structural evolution of plates.
与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。
Continental Crust is the inevitable product of formation and evolution of the Earth.
大陆地壳是地球形成演化的必然产物。
This study will provide important information for well understanding and probing into the nature and tectonic evolution of sub-continental lithospheric mantle since the Mesozoic-Cenozoic.
这一研究为了解华南内部中新生代以来陆下岩石圈地幔的属性以及构造演化提供了重要的信息。
Is only in recent geological evolution, this piece of land gradual subsidence, seawater intrusion was formed a continental shelf.
只是在最近的地质演变中，这片土地逐渐下沉，海水入侵才形成了大陆架。
The continental shelf are not immutable, and it along with the geological evolution of the Earth, has produced a constant slow and never-ending change.
大陆架并不是永远不变的，它随着地球地质演变，不断产生缓慢而永不停息的变化。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
根据基底性质分析，探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。
The Ehu intrusion is composed of a continental crust transformation type (S-type) granite and displays a textural and compositional evolution sequence.
鹅湖岩体为S型花岗岩，具有结构和成分演化序列。
Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.
江苏下扬子区的海相中—古生界构造演化经历了前扬子板块、稳定地台和西太平洋活动陆缘等三大阶段。
This has significant implications for TTG petrogenesis, I-type granite origin and continental crust evolution.
这对TTG岩石的成因、I型花岗岩的形成以及陆壳成分的演化都有着重要的意义。
The Lixian-Minxian foreland basin undertook abyssal-bathyal flysch deposition at its earlier evolution stage and continental molasse stage at its later evolution stage.
礼岷前陆盆地经历了早期深海—半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。
The Fujian continental crust originated in Archean era possesses a characteristic of multi-phase and multi-stage activity during its evolution.
晚太古宙和早元古宙是陆壳形成的主要时期，并已具现今板块活动特征。
The Fujian continental crust originated in Archean era possesses a characteristic of multi-phase and multi-stage activity during its evolution.
晚太古宙和早元古宙是陆壳形成的主要时期，并已具现今板块活动特征。
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