Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks   总被引：7，自引：0，他引：7  

Wu-Xian Li  Xian-Hua Li  Zheng-Xiang Li  Fa-Sheng Lou 《Gondwana Research》2008,13(3):288-301

Leucogranitic lenses are found within the Xiwan ophiolitic mélange in northeastern Jiangxi Province, South China. The leucogranites occur exclusively within the serpentinized peridotite unit of the ophiolite suite. SHRIMP U–Pb zircon dating results indicate that these granites were formed at 880 ± 19 Ma, and were overprinted by an Indosinian tectono-thermal event at ~ 230 Ma. The leucogranites are peraluminous (A/CNK = 1.0–1.24), characterized by high Al₂O₃ (14–18.33%) and Na₂O (6.5–10%) and clearly low εNd(T) values of 0.8 to − 3.9 compared with the other rock units of the ophiolite suite. On the basis of their REE characters, the leucogranites can be divided into three groups. Group I leucogranites show the most fractionated LREE-enrichment patterns (with La_N/Yb_N and La_N/Sm_N ratios of 30.1–75.0 and 2.3–3.9, respectively). Group II leucogranites have moderately fractionated LREE-enrichment patterns (with La_N/Yb_N and La_N/Sm_N ratios of 13.1–26.5 and 0.8–1.9, respectively). Group III leucogranites are characterized by obviously low total REE contents and flat REE patterns with significant positive Eu anomalies, probably due to small degrees of partial melting. All these leucogranites were likely formed by partial melting of sedimentary rocks from a marginal basin at the Yangtze side of the orogen, beneath a major thrust fault during the obduction of the ophiolite onto the continental crust. They are broadly similar to obduction-related granites within ophiolites identified in many places worldwide. Identification of the ca. 880 Ma obduction-type granites in the NE Jiangxi ophiolite provides a petrological constraint on the timing of the ophiolite obduction onto the continental crust. In combination with the termination of the Shuangxiwu arc magmatism at ca. 890 Ma, we interpret that the close of the Neoproterozoic back-arc basin and the termination of the continental amalgamation between the Yangtze and Cathaysia Blocks occurred at ca. 880 Ma.  相似文献   

Self-similar dynamics of a magnetized polytropic gas     

Wei-Gang Wang  Yu-Qing Lou 《Astrophysics and Space Science》2007,311(4):363-400

In broad astrophysical contexts of large-scale gravitational collapses and outflows and as a basis for various further astrophysical applications, we formulate and investigate a theoretical problem of self-similar magnetohydrodynamics (MHD) for a non-rotating polytropic gas of quasi-spherical symmetry permeated by a completely random magnetic field. Within this framework, we derive two coupled nonlinear MHD ordinary differential equations (ODEs), examine properties of the magnetosonic critical curve, obtain various asymptotic and global semi-complete similarity MHD solutions, and qualify the applicability of our results. Unique to a magnetized gas cloud, a novel asymptotic MHD solution for a collapsing core is established. Physically, the similarity MHD inflow towards the central dense core proceeds in characteristic manners before the gas material eventually encounters a strong radiating MHD shock upon impact onto the central compact object. Sufficiently far away from the central core region enshrouded by such an MHD shock, we derive regular asymptotic behaviours. We study asymptotic solution behaviours in the vicinity of the magnetosonic critical curve and determine smooth MHD eigensolutions across this curve. Numerically, we construct global semi-complete similarity MHD solutions that cross the magnetosonic critical curve zero, one, and two times. For comparison, counterpart solutions in the case of an isothermal unmagnetized and magnetized gas flows are demonstrated in the present MHD framework at nearly isothermal and weakly magnetized conditions. For a polytropic index γ=1.25 or a strong magnetic field, different solution behaviours emerge. With a strong magnetic field, there exist semi-complete similarity solutions crossing the magnetosonic critical curve only once, and the MHD counterpart of expansion-wave collapse solution disappears. Also in the polytropic case of γ=1.25, we no longer observe the trend in the speed-density phase diagram of finding infinitely many matches to establish global MHD solutions that cross the magnetosonic critical curve twice.   相似文献   

利用盐沼泥炭重建长江三角洲北部全新世中期海平面   总被引：2，自引：0，他引：2       下载免费PDF全文

战庆  王张华 《古地理学报》2014,16(4):548-556

根据对长江三角洲北部海安地区4个钻孔标志性沉积物(潮上带盐沼泥炭、高潮滩沉积)的年龄测定和高程测量,以及沉积物压实沉降量的分析研究,重建了本研究区全新世中期8.1～7.3 cal kyr BP和5.6～5.4 cal kyr BP的相对海平面位置。结果显示,8.1～7.3 cal kyr BP海平面缓慢上升1.46m,上升速率仅为0.2cm/yr, 与三角洲南部全新世早期海平面的快速上升(2cm/yr)形成鲜明对比,验证了冰盖控制下的全球海平面阶段性波动上升模式。对比长江三角洲地区海平面曲线发现,三角洲北部海平面曲线较南部低5～6m,长江三角洲海平面曲线与世界各地海平面曲线也存在明显差异,分析认为主要是由长江口地区的差异性沉降和中国东部边缘海的水均衡作用两个因素引起的。  相似文献   

Collisional interaction limits between dark matter particles and baryons in 'cooling flow' clusters     

Jian Hu  Yu-Qing Lou 《Monthly notices of the Royal Astronomical Society》2008,384(2):814-820

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基岩弹性刚度对土层地震反应的影响   总被引：4，自引：1，他引：3  

潘旦光  楼梦麟 《地震工程与工程振动》2004,24(4):158-163

将基岩上均匀、各向同性土层的地震反应,简化为置于弹性支座上的一维剪切梁模型进行分析。将地震激励假定为白噪声谱,在随机边界激励下,主要探讨了土层与基岩2种介质间的波阻抗比、波速比、土层厚度和阻尼特性对土层地震反应的影响。计算结果表明,对于一定的土层厚度,在一定阻尼比条件下,土层和基岩的阻抗比小到一定程度时,可以将基岩假定为刚性约束,而误差可以控制在一定的范围内。  相似文献   

土地利用变化时空模型的图谱方法--以黄河三角洲为例   总被引：12，自引：0，他引：12  

叶庆华  田国良  刘高焕  YE Jingmin  YAO Xin  LIU Qingsheng  LOU Weiguo  WU Shuguang 《地理学报(英文版)》2004,14(2):131-142

Changesinlandcoverandland-usehaveimpactsandimplicationsatlocal,regionalandglobalscalesbecauseofthewaytheyalterbiophysical,biogeochemicalandhydrologicalstatesandprocesses(Alcamoetal.,1996;Li,1996).Since1990,scientistsathomeandabroadhavebeenpayingattentiontoresearchesonland-useandland-coverchange(LUCC)(Turneretal.,1990;MeyerandTurner,1994),butresearchisnotenoughon"spaceandprocess"ofLUCC(Turneretal.,1995).Spatialrelationshipbetweenvariablesyethasnotbeenestablished(Bockstael,1996).Soitispara…  相似文献   

全国重要矿产资源潜力评价一些基本预测理论方法的进展     

肖克炎  娄德波  孙莉  李景朝  叶天竺 《吉林大学学报(地球科学版)》2013,43(4):1073-1082

全国25种重要矿产资源潜力评价工作是迄今为止投入最多的矿产预测评价工作,采用的技术方法是基于矿床模型的综合地质信息预测方法。预测工作针对矿产预测的基本问题,如地质工作的不平衡性、三维预测、定量预测与定性预测结合、地物化遥综合预测等问题进行有益探索,提出了新的解决方案。以矿产预测类型为纲,开展建造构造编图,将建造与成矿环境结合;通过矿产预测类型的成矿模式、预测要素研究构建定量预测模型;通过成矿地质体地质参数法预测实现二维到三维的定量预测。  相似文献   

长江口北支潮滩不同沉积微相有机地球化学元素分布^*          下载免费PDF全文

李琳  王张华  吴绪旭  高晓琴 《古地理学报》2013,15(1):95-104

利用在长江口崇明岛北支北四滧港（SY）、北堡港（BBG）以及新卫村（XW）潮滩获取的表层沉积物,测试总有机碳（TOC）、总氮（TN）及总硫（TS）含量,分析有机地球化学元素在潮滩微相的分布规律及影响因素,试图建立TOC/TN、TS/TOC等潮滩微相识别指标。研究结果显示,影响长江口潮滩TN、TS微相分布的重要因素为有机质含量及类型。在淤涨型潮滩,TOC/TN在高潮滩一般大于10,在中潮滩明显降至10以下;中潮滩植被带TS/TOC最高,平均值达0.063,其次为高潮滩互花米草带和中潮滩光滩（分别为0.055和0.054）,高潮滩芦苇带最低;TS-TOC一元线性回归斜率在高潮滩芦苇带呈现为显著低值,自高潮滩米草带向光滩,逐渐增大。在侵蚀型潮滩,TOC/TN从高潮滩到低潮滩均大于10,而且中、低潮滩的比值大于高潮滩,潮下带骤降至小于10;TS/TOC自陆向海逐渐增大,TS-TOC一元回归斜率高潮滩最低,中潮滩最高。另外,侵蚀型潮滩各微相的TS-TOC一元线性回归斜率均明显低于淤涨型潮滩。上述研究结果表明,长江口沉积物的TOC/TN和TS/TOC及TS-TOC一元线性回归斜率与潮滩沉积微相之间存在一定的关系,具有应用于全新世钻孔识别潮滩沉积物微相的潜力。  相似文献   

工程场地地震安评中加速度反应谱标准化问题的讨论   总被引：1，自引：1，他引：0  

楼梦麟  陈培德 《震灾防御技术》2012,7(2):121-129

文中计算了不同地震输入模式下的拱桥地震反应,讨论了输入指定地震波进行时域计算结果和按对应的反应谱进行计算所得结果之间的差异,特别分析了分别按地震波的实际反应谱和经过标定的反应谱计算得到的拱桥地震反应之间的不同.数值结果表明:在工程场地地震安全性评价中,采用标准反应谱的方式所提供的场地地震加速度参数,将会抹杀土层场地动力特性对地表地震动的影响.因此,按此地震动参数进行结构反应计算时,有时会低估结构的地震反应,留下结构抗震不安全的隐患.  相似文献   

长江口现代潮滩表层沉积物磁性特征和自生铁硫化物的分布^*   总被引：1，自引：1，他引：0       下载免费PDF全文

高晓琴  王张华  李琳  吴绪旭 《古地理学报》2012,14(5):673-684

以长江口崇明岛北支潮滩的3个潮滩为对象,在粒度测量和磁性分析的基础上,揭示了现代潮滩表层沉积物的磁性变化,探讨了磁性矿物、尤其是自生亚铁磁性矿物—硫复铁矿（Fe₃S₄）在潮滩沉积微相的分布规律及机制。研究结果表明：长江口潮滩表层沉积物的磁性特征由亚铁磁性矿物及超顺磁颗粒(SP)主导。淤积型中高潮滩磁铁矿以单畴(SD)和SP为主,侵蚀型潮滩的中低潮滩则更多假单畴/多畴(PSD/MD)晶粒,反映了水动力的分选及以细颗粒矿物溶解为主的早期成岩作用。此外,最东侧的北四滧港剖面潮上带—高潮滩芦苇带普遍存在自生亚铁磁性硫复铁矿,北堡港和新卫剖面的高潮滩也局部存在硫复铁矿,反映了本区高潮滩—潮上带丰富的有机质及细颗粒沉积物、加上有限的海水淹没时间,是早期成岩作用过程中生成硫复铁矿的主要机制。  相似文献