Stretching characteristics and its dynamic significance of the northern continental margin of South China Sea   总被引：5，自引：0，他引：5  

Zhang YunFan  Sun Zhen  Zhou Di  Guo XingWei  Shi XiaoBin  Wu XiangJie  Pang Xiong 《中国科学D辑(英文版)》2008,51(3):422-430

To investigate the thinning of the whole crust, and the contribution of the upper versus lower crust to the stretching since Cenozoic, we calculated the stretching factor of the northern margin of South China Sea with data such as whole crustal thickness, depth of Cenozoic sedimentary basement and the horizontal displacement of faults. An isometric line drawing on whole crustal stretching factor is then obtained. Along the seismic Line 1530 in Baiyun sag, we also calculated the stretching factors of the upper and lower crust. The results suggest that the whole crustal thickness decreases seaward while the whole crustal stretching factor increases from shelf to slope. The Moho upwells highest beneath where the crust is thinned most. The value of the whole crustal stretching factor ranges from 1.5 to 6. Two areas were thinned intensely: the center of Yinggehai Basin, and the Baiyun sag in the Pearl River Mouth Basin. The calculation of the upper and lower crustal stretching factors from DSP1530 in Baiyun sag shows that the original crust of Baiyun sag should be thinned before deformation. Its pre-Cenozoic evolution as well as tectonic position during Cenozoic might be responsible for that.  相似文献   

大陆裂谷作用的物理模拟     

孙珍  周蒂  曾佐勋  钟志洪 《地质科技情报》2000,19(1):23-26

裂谷作用的物理模拟是研究大陆裂谷系统的几何结构与动力学机制之间关系的一种直观有效的手段。对正向裂谷作用、斜向裂谷作用以及两期作用先后叠加模拟过程中,断裂系统发育的特征进行了综述。目前这些实验结果已被用于解释天然裂谷的形式,并根据断层方向的统计分析推导伸展向量的大致方向。  相似文献   

Structure of the Basin and Ridge System West of New Caledonia (Southwest Pacific): A Synthesis     

Y.?LafoyEmail author  I.?Brodien  R.?Vially  N.F.?Exon 《Marine Geophysical Researches》2005,26(1):37-50

Complementary to previous work mainly based on seismic interpretation, our compilation of geophysical data (multibeam bathymetry, gravity, magnetic and seismic) acquired within the framework of the ZoNéCo (ongoing since 1993) and FAUST (1998–2001) programs enables us to improve the knowledge of the New Caledonia Basin, Fairway Basin and Fairway Ridge, located within the Southwest Pacific region. The structural synthesis map obtained from geophysical data interpretation allows definition of the deep structure, nature and formation of the Fairway and New Caledonia Basins. Development of the Fairway Basin took place during the Late Cretaceous (95–65 Ma) by continental stretching. This perched basin forms the western margin of the New Caledonia Basin. A newly identified major SW–NE boundary fault zone separates northern NW–SE trending segments of the two basins from southern N–S trending segments. This crustal-scale fault lineament, that we interpret to be related to Cretaceous-early Cainozoic Tasman Sea spreading, separates the NW–SE thinned-continental and N–S oceanic segments of the New Caledonia Basin. We can thus propose the following pattern for the formation of the study area. The end of continental stretching within the Fairway and West Caledonia Basins ( 65–62 Ma) is interpreted as contemporaneous with the onset of emplacement of oceanic crust within the New Caledonia Basin’s central segment. Spreading occurred during the Paleocene (62–56 Ma), and isolated the Gondwanaland block to the west from the Norfolk block to the east. Finally, our geophysical synthesis enables us to extend the structural Fairway Basin down to the structural Taranaki Basin, with the structural New Caledonia Basin lying east of the Fairway Basin and ending further north than previously thought, within the Reinga Basin northwest of New Zealand.  相似文献   

Post-entrapment modification of fluid inclusions due to overpressure: evidence from natural samples   总被引：5，自引：0，他引：5  

A. J. BARKER 《Journal of Metamorphic Geology》1995,13(6):737-750

Abstract Effects of post-entrapment fluid-inclusion modification are examined with reference to retrogression-related quartz veins from the Caledonian, Øse Thrust, northern Norway. The inclusions occur in secondary trails, and contain high-density hypersaline aqueous fluids. On morphological characteristics, they are subdivided into, Type A: elongate, ellipsoidal and/or irregular inclusions, and Type B: more equant, regular, and/or negative crystal form. With reference to previous research on post-entrapment modification of inclusions in quartz it is proposed that Type A inclusions experienced little or no post-entrapment modification, whereas Type B inclusions show features characteristic of post-entrapment permanent inelastic stretching and/or leakage. This produces increased homogenization temperatures ( T _h), associated with increased inclusion volume and lowering of density, whilst maintaining constant salinity. The similarity of data for degree of fill and salinity between Type A and Type B inclusions indicates that Type B inclusions have primarily modified by stretch rather than leakage. However, the spread towards slightly larger volume of vapour in Type B inclusions suggests that some leakage has also occurred. Because stretched and/or partially leaked inclusions have increased T _h, isochore projections significantly underestimate trapping pressure ( P _t) relative to unmodified inclusions. Therefore, recognition of post-entrapment inclusion modification due to overpressure is crucial to avoid misinterpretation of data, but has considerable potential for constraining the detail of P-T trajectories of individual rocks. On this basis, rocks from the Øse Thrust zone, north Norway, are shown to have experienced rapid uplift on a 'clockwise' P-T-t path during the final stages of Caledonian (Scandian) orogenesis.  相似文献   

新疆哈密黄山韧性挤压带超塑性拉伸砾石的特征及形成机制   总被引：2，自引：0，他引：2  

徐兴旺  马天林  孙立茜  李贵书 《地球学报》1996,17(3):276-281

新疆哈密黄山韧性挤压带变形砾石具超塑性拉伸的特征，变形砾石平均棉球体长短轴比（Ｘ／Ｚ）大于１０．变形砾石的微观构造、超微观构造、石英组构、及变形砾石拉伸量与砾内石英颗粒轴比（Ｘ／Ｚ）和砾内面理间隔（Ｄ）关系等的综合研究表明，挤压及其所导致的砾内矿物的细粒化和拉伸及砾内面理间隔的减小是砾石超塑性拉伸的重要变形机制。变形砾石粒度大小和岩性对砾石拉伸变形具一定的敏感性。另外，随着拉伸应变量的增大，硅质岩砾石石英组构有从Ｖ型极密、小圆环带、交叉环带向Ⅷ型极富和Ⅰ型极密演化的特征。  相似文献   

Improved Geological Interpretation Using Landsat TM Data in Lancang-Jinghong Area, Yunnan Province, China     

BassamFAIBassam 《中国地质大学学报(英文版)》2003,14(1):52-58

Landsat TM digital spectral data of Lancang-Jinghong area (Yunnan Province) has been used for the purpose of geological interpretation. To meet this object, different image processing tech-niques including selected band color composites, principal component analysis and IHS decorrelation stretching are used to improve the discrimination of different lithologicai and structural features in the area. It was found that IHS decorrelation stretching images obtained from the transformation of false color composite 741 (in red, green and blue) provided the best results based on the original data. By combining the characteristics of images produced by different approaches and other canonically trans-formed images with available geological data and surface observations, the geological interpretation could be done with satisfactory degree of accuracy.  相似文献   

A Fourteen-Year Climatology of the Southwest Vortex in Summer   总被引：4，自引：0，他引：4       下载免费PDF全文

FU Shen-Ming  ZHANG Jing-Ping  SUN Jian-Hua  SHEN Xin-Yong 《大气和海洋科学快报》2014,7(6):510-514

Statistical studies were conducted on the southwest vortex（SWV） during the summers of 2000–13 using high-resolution reanalysis data with a horizontal resolution of 0.5°× 0.5°. A total of 578 SWVs were detected, with a maximum interannual frequency of 55. The variation of the interannual frequency featured a period of around six years. The most active period of SWVs was early July and the maximum occurrence of SWVs appeared in early morning（0200–0800 Beijing Standard Time（BST））. Most of the SWVs were short-lived, with only 66 cases（11.4%） lasting for more than 24 h. In addition, the moving tracks and three-dimensional shape of long-lived（≥ 36 h） SWVs are also presented. For those SWVs that lasted for more than 12 h, four types of SWVs（Types I–IV） were identified using a new method, and the results indicated that the dynamical and thermodynamical conditions before the formation of SWVs are effective indicators of the subsequent evolution of the vortex and associated severe weathers. Moreover, a further level of classification was also constructed for Type II SWVs, which accounted for the largest proportion out of Types I–IV, and the results indicated that the lifespan, radius and maximum 6-h precipitation were all closely related to the intensity of precipitation before the formation of SWVs.  相似文献   

高精度时间间隔测量技术与方法   总被引：31，自引：0，他引：31  

张延  黄佩诚 《天文学进展》2006,24(1):1-15

时间间隔测量技术,尤其是高精度的时间间隔测量技术意义重大。不论是电信通讯、芯片设计等工程实践,还是原子物理、天文观测实验等理论研究,以及激光测距、卫星定位等航天军事技术,都离不开高精度的时间间隔测量技术。经过几十年的研究,目前已经有多种测量方法。在阐明插值原理之后,依次介绍了直接计数法、扩展法、时间幅度转换法、游标法、抽头延迟线法和差分延迟线法等主要方法。然后对影响测量的几个因素,包括非线性和不定态作了讨论。针对这些不良影响,还探讨了一些提高精度和稳定度的方法,比如非线性校正、PLL(Phase Lock Loop)和DLL (Delay Lock Loop)技术。最后,对时间间隔测量技术的前景作了展望。  相似文献   

大别山北缘西段双桥中生代火山岩地球化学及锆石U-Pb同位素年代学   总被引：1，自引：0，他引：1  

杨梅珍  曾键年  任爱琴  陆建培  覃永军  李法岭 《岩石矿物学杂志》2012,31(2):133-144

首次对大别山北缘西段(河南省境内)中生代火山岩进行了锆石原位U-Pb同位素测年。结果表明,罗山县双桥火山岩集中区石英安山岩锆石LA-ICP-MS U/Pb年龄为133.1±1.5 Ma,与大别东段中生代火山岩主体毛坦厂组的时代一致,属早白垩世,稍早于或与大别山区大规模花岗岩岩基侵位时代相同;与长江中下游地区的宁芜和庐枞盆地火山岩喷发时间同步,可能同属中国东部中生代巨量岩浆活动的重要组成部分,与太平洋板块斜向俯冲引起的大陆岩石圈重力不稳而产生的拆沉导致岩石圈强烈减薄深部动力学过程相联系。大别山西段早白垩世火山岩属高钾钙碱性系列粗安岩-英安岩-流纹岩组合。中酸性火山岩显示轻稀土元素富集、重稀土元素强烈亏损、弱或基本无负Eu异常的稀土元素配分模式以及高Sr低Yb特征,反映岩浆部分熔融源区残余有石榴石,说明当时存在加厚的成熟陆壳。高(87Sr/86Sr)i(0.707 56)、极低的εNd(t)(-20.1)和大离子亲石元素富集、高场强元素Nb、Ta明显亏损,显示岩浆源区的壳源性质。以上特征反映大别山地区该时期岩石圈伸展程度和软流圈上涌规模远不如长江中下游同时期以幔源为主的中基性火山岩发育的宁芜和庐枞地区。  相似文献   

利用宽谱系岩墙群进行靶区定位的数值方法——以新疆南阿拉套山为例     

郭晶  罗照华  刘晓  姜会营 《中国地质》2013,40(2):423-429

本文介绍一种利用宽谱系岩墙群的空间展布特征进行靶区定位的数值方法.基于透岩浆流体成矿理论,岩浆-屏蔽层强相互作用过程中将涌现最大主压应力分布在竖直方向的近场应力场.在这种条件下,屏蔽层中的裂隙系统不同于传统矿田构造学描述的裂隙系统.依岩浆上升速率及屏蔽层岩石学结构和力学性质变化,屏蔽层中可出现不同类型的同成矿裂隙系统,后者往往被成矿期的脉岩充填.由于应力中心的作用力强度大于远离应力中心的部位,自生长裂隙和先存裂隙的密度呈现规律性的空间变化.这种变化控制了含矿流体的运动学特征.因此,可以将岩墙密度和延伸方向数作为定量化指标揭示含矿流体大规模聚集的空间位置,后者也是成矿作用的潜在发生部位.用滑动平均法绘制岩墙分布密度图和岩墙延伸方向密度图,将极密区作为有利找矿靶区,分析结果与地质学方法的预测结果高度相似.因此,可以认为本文提供的靶区圈定方法是一种简便有效的方法.  相似文献