柳河地区晚太古代高级变质区地质特征及变质作用     

王永胜  曲永贵 《吉林地质》1998,17(4):65-75

笔者在１：５万区调工作中,于吉林省柳河地区首次发现了高级变质区,其变质程度达到麻粒岩相。通过野外地质观察,薄片研究,放射性同位素,ｐ－Ｔ－ｔ轨迹等方法和手段,对该区的变质时代,变质阶段,变质温压及构造环境等方面做了较深入的研究,并综合分析了该区的变质作用。  相似文献   

试论陆内型造山作用──以秦岭-大别山造山带为例          下载免费PDF全文

赵宗溥 《地质科学》1995,(1):19

 板块构造学说的大陆碰撞作用和槽台学说的地槽回返作用不能解释秦岭-大别山造山带的成因机制。壳幔拆离构造导致陆内A型俯冲是陆内型造山作用的成因机制。  相似文献   

On the hydrodynamic behavior of supercooled water drops interacting with columnar ice crystals     

R. J. Schlamp  H. R. Pruppacher 《Pure and Applied Geophysics》1977,115(4):805-843

A numerical evaluation of the complete Navier-Stokes equations of motion for steady-state, incompressible flow past an infinite circular cylinder is given in terms of the stream function, vorticity, and pressure distribution past such bodies. A method is described which allows use of these flow characteristics: (1) to approximate the characteristics of air flow past hexagonal columnar ice crystals falling under gravity at terminal velocity in air, (2) to compute the trajectory of supercooled cloud drops relative to such ice crystals, and (3) to determine the efficiency with which short columnar ice crystals and needle shaped ice crystals collide with supercooled cloud drops. It is found that for all columnar type ice crystals riming is negligible if the cloud drop size is less than 5 m, and that for riming to commence short columnar crystals must have diameters larger than 50 m, while needle crystals must have diameters larger than 40 m. It is further shown that the collision efficiency cut-offs at the small drop radius and at the large drop radius end of the collision efficiency diagram can be explained on the basis of the cloud drop trajectories for these drop size ranges.  相似文献   

桐柏山-大别山的地体构造特征和构造演化   总被引：4，自引：0，他引：4       下载免费PDF全文

马宝林 《地震地质》1991,13(1):33-42,T001

本文讨论了桐柏山-大别山的地质构造特征。对该区三个地体进行了研究,指出:南部随州-广济高压浅变质地体具有俯冲杂岩性质;北部北淮阳高压浅变质地体中、西段具有俯冲杂岩性质,东段具有构造混杂岩特征;中部桐柏-大别山地体早期是洋盆中的大陆地壳残块,后期演化成岛弧。在加里东或海西-印支时期三地体先后碰撞造山。随州-广济地体和北淮阳地体分别向北、向南逆掩或推覆到桐柏-大别地体之上  相似文献   

西藏阿里地区北部新生代火山岩—兼论陆内俯冲作用   总被引：9，自引：4，他引：9  

邓万明 《岩石学报》1989,5(3)

本文研究了新南藏北昆仑山南侧新生代火山岩的地质学、岩石学和主要元素、痕量元素地球化学特征;划分出以新第三纪喷发为主的碱性火山岩带(南带)和与之伴随的第四纪钙碱性火山岩带(北带);用塔里木大陆岩石圈向青藏高原下面的俯冲机制解释了本区火山岩的成因,并且认为陆内俯冲作用不但可以说明中国西部诸山系的近期上升,而且可以运用于所有地壳厚度异常的碰撞带,因而具有普遍的意义。作者划分出具有不同地质特色的昆仑山型和喜马拉雅型两种陆内俯冲模式。  相似文献   

Has the plate boundary shifted from central Hokkaido to the eastern part of the Sea of Japan?     

Naoko Kato  Hiroshi Sato  Masayuki Orito  Kazuomi Hirakawa  Yasutaka Ikeda  Tanio Ito   《Tectonophysics》2004,388(1-4):75

A NS trending Cenozoic fold-and-thrust belt has developed in the western part of the Hidaka Collision Zone (HCZ), central Hokkaido, Japan. A quantitative estimation of the late Cenozoic convergence rate at the front of the Hidaka thrust system is important in revealing the plate tectonic framework around northern Japan. High-resolution seismic reflection profiling across the active fault-related folds was carried out to ascertain the temporal change in the crustal shortening rate. Overlapping ramp anticlines and growth folds within thrust sheets were examined using balanced cross-sections combined with industry seismic and drilling data. The rate of shortening was examined using a 3.5 Ma horizon and late Quaternary horizons at 115 and 41 ka. These horizons show that the convergence rate of the Hidaka thrust system has not decreased during the last 3.5 Ma. This suggests that the plate boundary between the Eurasian (Amurian) and North American (Okhotsk) plates has not jumped from the central part of Hokkaido to the eastern part of the Sea of Japan since 3.5 Ma and that a significant amount of plate convergence is still being absorbed in the Hidaka Collision Zone.  相似文献   

在板块边缘的冲撞地区重力场的求定   总被引：7，自引：2，他引：7  

陈俊勇  刘允诺 《测绘学报》1994,23(4):241-246

在陆地上，板块边的冲撞地区一般都是呈现地形复杂，地表和地下的质量分布不均衡、有强烈的地壳运动和构造运动，因此，该地区的重力场（重力异常、垂线偏差，大地水准面）变化剧烈。对它的归算和推估都需要作特殊的考虑。本文以位于欧亚板块和印度板块边缘冲撞地区的珠穆朗玛峰测区的重力场求定为例，进行讨论。  相似文献   

蓝田构造窗   总被引：11，自引：0，他引：11       下载免费PDF全文

徐树桐  孙枢 《地质科学》1993,28(2):105-116

蓝田构造窗位于安徽省南部上溪辟(相当于板溪群)中。组成构造窗的地层为震旦系和部分下古生界,它们以断层与周围浅变质岩接触。浅变质岩包括构造混杂岩、复理石浊积岩、钙碱性火山岩和相应的沉积岩以及前震旦纪碎屑岩四种岩石单位,它们是不同构造背景下的产物,在扬子板块与华南板块碰撞造山过程中聚集到一起的。据此可识别出,以往所说的蓝田盆地实际上是一个构造窗。  相似文献   

亚洲东部新生代碰撞构造:构造逃逸还是单剪—旋转?     

薛锋 《地球物理学进展》1993,(1)

碰撞构造学是当前大陆构造研究的重要方面,是国际构造学界关注的热点.简要综述了这一领域里众所注目的一场争论,即在印度—欧亚碰撞中欧亚板块的变形究竟以大陆块体的构造逃逸还是以单剪体制下的块体旋转构造样式进行.  相似文献   

Reliability analysis of wake-induced collision of flexible risers     

《Applied Ocean Research》2017

Collision between risers is an important design and operational concern, especially in deep water since the probability of collision tends to increase as the riser length increases. Riser collision is due to the joint effects of many processes, i.e. environmental loads, hydrodynamic interference and surface floater motions and the most of them are stochastic processes. This paper provides an approach for estimating the failure probability of riser collision by considering these joint effects and their stochastic nature. Firstly, a procedure for establishing the distribution function of the extreme minimum relative distance between two risers is introduced based on simulation tools and statistical data. Numerical simulation is performed to compute the minimum distance between risers for a given duration. Repeated simulations are applied so that the extreme value distribution can be established. Secondly, reliability analysis is performed by considering the uncertainties of input parameters related to environmental loads and riser system. The collision probability is calculated based on both the First/Second Order Reliability Method and the Monte Carlo simulation techniques.  相似文献