Space geodesy in geodynamic studies: Recent movements in the Zeya-Bureya Basin     

A. I. Miroshnichenko  A. P. Sorokin  V. A. San’kov  A. V. Lukhnev  S. V. Ashurkov  A. T. Sorokina  N. I. Panfilov  M. A. Serov  S. I. Sherman 《Russian Journal of Pacific Geology》2008,2(1):64-71

The Amur-Zeya geodynamic test ground was set up in 2000 to study recent intracontinental crustal deformations. The velocity field calculations for the period of 2000 to 2003 describe three movements scales. The general level is characterized by the vectors of IGS sites in the eastern part of Asia, the BLAG (Blagoveshchensk) site included. The southeast movement of the IRKT (Irkutsk) site of the stable Siberian Platform is indicative of deformations in the northeastern part of the Amur Plate. Measurement data on the regional near-latitudinal profile Blagoveshchensk-Sutara, which crosses the Nizhnyaya Zeya Basin, demonstrate a southwestward displacement of the Badzhal-Bureya-Lesser Khingan block relative to the North China block. The dynamic effect of the convergent boundary between the Amur and Okhotsk Sea plates is assumed to extend inland also involving the Zeya-Bureya Basin area. The measurements on the local geodynamic test site relate the deformations of buildings and constructions in the Settlement of Konstantinovka to the mobility of basement faults in the southern part of the Nizhnyaya Zeya Basin. Aseismic deformations are determined by slow horizontal tectonic movements in the junction zone of NNE-trending structures of the latter basin and near-latitudinal faults of the Khailar-Xunhei Belt.  相似文献   

Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton. Evidence for a 2.1 Ga thermal and tectonic event in the Fuping Massif     

P. Trap  M. Faure  W. Lin  O. Bruguier  P. Moni 《Journal of Structural Geology》2008,30(9):1109-1125

Structural analysis along with ⁴⁰Ar–³⁹Ar and U–Pb datings in the Fuping massif provide new insight into the evolution of the eastern part of the Trans-North China Belt (North China Craton), from 2.7 Ga to 1.8 Ga. D1 is responsible for the development of a dome-and-basin structure coeval with crustal melting giving rise to migmatite and Nanying gneissic granites at 2.1 Ga. This dome-and-basin architecture resulted from the interference between a N–S compression of a weak ductile crust and gravity-driven vertical flow, in a high thermal regime. The next events involved flat lying ductile thrusting (D2) and normal faulting (D3) dated at around 1880 Ma and 1830 Ma, respectively. The D2 and D3 events belong to the Trans-North China Orogeny that results in the final amalgamation of the North China Craton. The D1 deformation is considered as evidence for an earlier orogen developed around 2.1 Ga prior to the Trans-North China Orogeny. The change in the deformation style between the 2.1 Ga and 1.8 Ga could be viewed as a consequence of the cooling of the continental crust in the North China Craton.  相似文献   

地幔Sr-Nd-Pb同位素演化的综合模型与n维同位素空间 “地幔面”的地质意义     

隋建立  樊祺诚  赵勇伟  杜星星 《岩石学报》2008,24(11):2615-2620

在n维的Sr-Nd-Pb同位素空间中,几乎所有的大洋中脊玄武岩（MORB）和洋岛玄武岩（OIB）都落在一个虚拟平面上,被称为“地幔面（mantle plane）”。“地幔面”描述了大部分玄武岩的同位素地球化学特征,是最重要的、也是最早提出的地幔动力学演化特征之一,但是长期以来关于“地幔面”的内涵和意义并不清楚。本文通过一个综合模型,反演受岩浆作用控制的地幔微量元素（包括各种同位素母体元素）分异、Sr—Nd—Pb同位素演化,并推导出地幔Sr-Nd-Pb同位素演化的二元参数方程形式。模型表明,通过部分熔融向地壳输出相对富硅、富碱的物质成分,是地幔长期演化的主要特点,这个过程受到两个参数一部分融融程度（F）和岩浆分离的时间（t）-的控制,即n维参数可化为2维,因此在n维同位素空间出现“地幔面”的特征。壳源物资循环,能够使局部地幔偏离“地幔面”,就地幔总体统计特征而言,地壳混染的比例很低,不同的统计数据显示大约1％～6％的系统偏差,即可能的地壳混染程度;进一步模拟,可能作出更加精确的估算。  相似文献   

Tectonic Evolution of Tertiary Basins in circum-Pacific Belt of China and Their Geodynamic Setting   总被引：1，自引：0，他引：1  

Li Sitian Yang Shigong Xie XinongFaculty of Earth Resources  China University of Geosciences  Wuhan  《中国地质大学学报(英文版)》1997,(1)

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New palaeomagnetic results from the Kerguelen Islands     

Bernard Henry  Claude Plessard 《Geophysical Journal International》1997,128(1):73-83

New palaeomagnetic analyses have been carried out in the Kerguelen Islands on 32 lava flows of well-established age (20–22 Ma). Combined with previous studies, they yield a reliable pole for the Lower Miocene for the Antarctic plate: N = 59 flows. 349.9°E, 83.5°S, A⁹⁵= 6.1°. A reversal sequence reversed-normal has been identified in the Port Jeanne d'Arc section.  相似文献   

重力场的潮汐变化观测及其研究   总被引：6，自引：1，他引：6  

孙和平  许厚泽  徐建桥  柳林涛 《地球科学进展》2000,15(1):53-57

基于我国武汉超导重力仪长周期序列潮汐观测数据,研究了重力场潮汐变化特征,精密确定了地球潮汐常数,讨论了重力观测中的海潮负荷和大气效应问题;根据地球自由核章动在周日重力潮汐观测中的共振效应确定了自由核章动的复本征周期和品质因子Q值,研究了极移重力效应;并对进一步利用重力潮汐观测研究地球物理问题进行了讨论。  相似文献   

Gravity analysis offshore the Canary Islands from a systematic survey     

A. Carbó  A. Muñoz-Martín  P. Llanes  J. Álvarez 《Marine Geophysical Researches》2003,24(1-2):113-127

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Accessing Australian geodynamic information: The AGCRC website     

S. J. D. Cox  K. D. Covil 《Australian Journal of Earth Sciences》2013,60(4):613-622

The Australian Geodynamics Cooperative Research Centre (AGCRC) website <http://www.agcrc. csiro.au/> provides the main integrated presentation of the results of AGCRC research. It hosts a systematic presentation of project summaries, publication abstracts, regionally organised geodynamic syntheses and a GIS database containing a large number of broad‐scale earth science datasets from the Australian region, which are presented through an interactive map viewer. Effective interfaces are required to make the variety of content accessible to users. In particular, maintaining effective hyperlinking for a large and growing set of pages was a significant challenge. We found that by developing effective indexing tools we were able to apply a uniform technology to attack these problems. The index included both the full text of the pages from the website and also specific index terms of metadata. The metadata schema was designed to support both generalised discovery through a search interface and also to allow hyperlinks to be included automatically in pages by the server, so that the user could browse in a richly cross‐linked framework. It was necessary to manage textual and numeric data within the same framework because even the textual documents were generally tied to geospatial locations identified by their geographical coordinates. This required extensions to standard index and search tools, including the development of complete new indexing software. To assist the user in accessing the index, we provided a variety of user interfaces specialised for different themes in the website. For example, publication lists are generated in a conventional layout, and geospatial datasets are presented through an interactive map viewer and query system. The latter also demonstrated how visualisation tools for geospatial data can be provided in the web‐browser interface.  相似文献   

The Tajik Basin: A composite record of sedimentary basin evolution in response to tectonics in the Pamir     

James B. Chapman  Barbara Carrapa  Peter G. DeCelles  James Worthington  Nicoletta Mancin  Miriam Cobianchi  Marius Stoica  Xin Wang  Mustafo Gadoev  Ilhomjon Oimahmadov 《Basin Research》2020,32(3):525-545

Investigation of a >6-km-thick succession of Cretaceous to Cenozoic sedimentary rocks in the Tajik Basin reveals that this depocentre consists of three stacked basin systems that are interpreted to reflect different mechanisms of subsidence associated with tectonics in the Pamir Mountains: a Lower to mid-Cretaceous succession, an Upper Cretaceous–Lower Eocene succession and an Eocene–Neogene succession. The Lower to mid-Cretaceous succession consists of fluvial deposits that were primarily derived from the Triassic Karakul–Mazar subduction–accretion complex in the northern Pamir. This succession is characterized by a convex-up (accelerating) subsidence curve, thickens towards the Pamir and is interpreted as a retroarc foreland basin system associated with northward subduction of Tethyan oceanic lithosphere. The Upper Cretaceous to early Eocene succession consists of fine-grained, marginal marine and sabkha deposits. The succession is characterized by a concave-up subsidence curve. Regionally extensive limestone beds in the succession are consistent with late stage thermal relaxation and relative sea-level rise following lithospheric extension, potentially in response to Tethyan slab rollback/foundering. The Upper Cretaceous–early Eocene succession is capped by a middle Eocene to early Oligocene (ca. 50–30 Ma) disconformity, which is interpreted to record the passage of a flexural forebulge. The disconformity is represented by a depositional hiatus, which is 10–30 Myr younger than estimates for the initiation of India–Asia collision and overlaps in age with the start of prograde metamorphism recorded in the Pamir gneiss domes. Overlying the disconformity, a >4-km-thick upper Eocene–Neogene succession displays a classic, coarsening upward unroofing sequence characterized by accelerating subsidence, which is interpreted as a retro-foreland basin associated with crustal thickening of the Pamir during India–Asia collision. Thus, the Tajik Basin provides an example of a long-lived composite basin in a retrowedge position that displays a sensitivity to plate margin processes. Subsidence, sediment accumulation and basin-forming mechanisms are influenced by subduction dynamics, including periods of slab-shallowing and retreat.  相似文献   

中-新生代东北和华北的洋陆转换作用     

杨文采 《地质论评》2022,68(1):2022020013-2022020013

本文对西太平洋的洋-陆转换作用进行探讨。西太平洋洋-陆转换带在中国东部可分为华南、华北-黄海和东北3个区段。东北地区中-新生代洋-陆转换作用涉及古今太平洋板块和蒙古—鄂霍茨克洋板块两方面俯冲作用的影响,产生大面积中基性岩浆和火山活动,从侏罗纪一直延伸到现在。不同于东北和华南地区,华北-黄海有克拉通型的岩石圈,在晚侏罗世—新近纪因为太平洋板块的大角度旋转造成软流圈低黏度物质上涌,和地壳拉张与幔源岩浆的底侵,造成上地壳裂谷型沉积盆地。燕山地区在侏罗纪与东北地区类似,有强烈的软流圈上涌和岩石圈岩石部分熔融,产生强烈岩浆活动。在白垩纪到新生代,因为蒙古—鄂霍茨克洋闭合和太平洋板块大角度旋转,发生沿蒙古—鄂霍茨克洋的转换断层的拉张,产生从南蒙古过锡林浩特的NW向玄武质岩浆和火山带。洋-陆转换带不同区段有不同的动力学作用演化过程,与先期岩石圈的性质、大洋板块俯冲带的分布、方向变化和俯冲持续时间、以及后期俯冲带后撤作用都有密切关系。洋-陆转换作用的统一后果是大陆的增生,但是不同区段大陆增生和物质运动的模式是不一样的。  相似文献