Geophysical investigations of crust-scale structural model of the Qiongdongnan Basin, Northern South China Sea   总被引：2，自引：0，他引：2  

Ning Qiu  Zhenfeng Wang  Hui Xie  Zhipeng Sun  Zhangwen Wang  Zhen Sun  Di Zhou 《Marine Geophysical Researches》2013,34(3-4):259-279

Rifting of the Qiongdongnan Basin was initiated in the Cenozoic above a pre-Cenozoic basement, which was overprinted by extensional tectonics and soon after the basin became part of the rifted passive continental margin of the South China Sea. We have integrated available grids of sedimentary horizons, wells, seismic reflection data, and the observed gravity field into the first crust-scale structural model of the Qiongdongnan Basin. Many characteristics of this model reflect the tectonostratigraphic history of the basin. The structure and isopach maps of the basin allow us to reconstruct the history of the basin comprising: (a) The sediments of central depression are about 10 km thicker than on the northern and southern sides; (b) The sediments in the western part of the basin are about 6 km thicker than that in the eastern part; (c) a dominant structural trend of gradually shifting depocentres from the Paleogene sequence (45–23.3 Ma) to the Neogene to Quaternary sequence (23.3 Ma–present) towards the west or southwest. The present-day configuration of the basin reveals that the Cenozoic sediments are thinner towards the east. By integrating several reflection seismic profiles, interval velocity and performing gravity modeling, we model the sub-sedimentary basement of the Qiongdongnan Basin. There are about 2–4 km thick high-velocity bodies horizontal extended for a about 40–70 km in the lower crust (v > 7.0 km/s) and most probably these are underplated to the lower stretched continental crust during the final rifting and early spreading phase. The crystalline continental crust spans from the weakly stretched domains (about 25 km thick) near the continental shelf to the extremely thinned domains (<2.8 km) in the central depression, representing the continental margin rifting process in the Qiongdongnan Basin. Our crust-scale structural model shows that the thinnest crystalline crust (<3 km) is found in the Changchang Sag located in the east of the basin, and the relatively thinner crystalline crust (<3.5 km) is in the Ledong Lingshui Sag in the west of the basin. The distribution of crustal extension factor β show that β in central depression is higher (>7.0), while that on northern and southern sides is lower (<3.0). This model can illuminate future numerical simulations, including the reconstruction of the evolutionary processes from the rifted basin to the passive margin and the evolution of the thermal field of the basin.  相似文献   

Structural differences between the western and eastern Qiongdongnan Basin: evidence of Indochina block extrusion and South China Sea seafloor spreading   总被引：1，自引：0，他引：1  

Cuimei Zhang  Zhenfeng Wang  Zhipeng Sun  Zhen Sun  Jianbao Liu  Zhangwen Wang 《Marine Geophysical Researches》2013,34(3-4):309-323

Located at the intersection between a NW-trending slip system and NE-trending rift system in the northern South China Sea, the Qiongdongnan Basin provides key clues for us to understand the proposed extrusion of the Indochina Block along with Red River Fault Zone and extensional margins. In this paper we for the first time systematically reveal the striking structural differences between the western and eastern sector of the Qiongdongnan Basin. Influenced by the NW-trending slip faults, the western Qiongdongnan Basin developed E–W-trending faults, and was subsequently inverted at 30–21 Ma. The eastern sector was dominated by faults with NE orientation before 30 Ma, and thereafter with various orientations from NE, to EW and NW during the period 30–21 Ma; rifting display composite symmetric graben instead of the composite half graben or asymmetric graben in the west. The deep and thermal structures in turn are invoked to account for such deformation differences. The lithosphere of the eastern Qiongdongnan Basin is very hot and thinned because of mantle upwelling and heating, composite symmetric grabens formed and the faults varied with the basal plate boundary. However, the Southern and Northern Uplift area and middle of the central depression is located on normal lithosphere and formed half grabens or simple grabens. The lithosphere in the western sector is transitional from very hot to normal. Eventually, the Paleogene tectonic development of the Qiongdongnan Basin may be summarized into three stages with dominating influences, the retreat of the West Pacific subduction zone (44–36 Ma), slow Indochina block extrusion together with slab-pull of the Proto-South China Sea (36–30 Ma), rapid Indochina block extrusion together with the South China Sea seafloor spreading (30–21 Ma).  相似文献   

西藏甲玛铜多金属矿床深部斑岩矿体找矿突破及其意义   总被引：7，自引：0，他引：7  

唐菊兴  郑文宝  陈毓川  王登红  应立娟  秦志鹏 《吉林大学学报(地球科学版)》2013,43(4):1100-1110

甲玛铜多金属矿是西藏冈底斯成矿带中东段勘查程度最高、成矿元素与矿体类型复杂的超大型斑岩-矽卡岩型矿床。通过4年多、近350 个钻孔的验证,不仅实现了矽卡岩矿体的找矿突破,同时在0-40线深部发现了产于二长花岗斑岩与石英闪长玢岩中的斑岩钼（铜）矿体,建立了“四位一体”的找矿勘查模式。斑岩矿体赋存标高一般处于4 600 m以下,矿体走向NW-SE,倾向NE,近直立,矿体垂向延伸大于350 m;斑岩矿石以发育细脉-浸染状、网脉状构造为特征;矿石中的矿石矿物主要为黄铜矿与辉钼矿,少见斑铜矿;脉石矿物主要为石英。初步查明:与铜矿化有关的含矿岩体主要为偏中性的石英闪长玢岩,蚀变以典型的细粒热液黑云母交代角闪石斑晶和基质而成的黑云母化蚀变为主;与钼矿化有关的含矿岩体主要为二长花岗斑岩,蚀变以硅化为主,次为绿帘石化、泥化和钾化。斑岩体与碳酸盐岩接触带常产出厚度超过200 m的巨厚矽卡岩矿体,且在岩体一侧有内矽卡岩产出。甲玛深部斑岩矿体的发现不仅证实了“斑岩-矽卡岩型”的矿床成因观点,而且完善了甲玛矿床成矿模式与勘查模型。  相似文献   

大震作用下板式楼梯框架弹塑性地震反应分析     

敬艳梅  张新培  田志鹏 《世界地震工程》2012,28(1):69-80

有关大震作用下楼梯与框架共同工作方面的研究还很少,采用结构有限元软件Midas/Gen,对一个5层钢筋混凝土现浇板式楼梯框架办公楼模型进行了弹塑性分析,对模型在大震作用下的受力情况进行了详细研究.通过对楼梯和框架共同工作性能的研究,并与不考虑楼梯影响的框架的工作性能进行了对比,分析了板式楼梯框架的失效机制和受力特点,指出了楼梯与框架共同工作时的受力不利部位.结果表明:楼梯相较于框架梁柱是模型的薄弱部位;模型的失效是从楼梯发展到框架,由下层发展到上层.最后根据模型的失效机制特点提出了相应的抗震措施.  相似文献   

地区间贸易流量的产业—空间模型构建与应用   总被引：9，自引：1，他引：8  

刘卫东  刘红光  范晓梅  陈杰  唐志鹏 《地理学报》2012,67(2):147-156

通过深入剖析区域间经济联系的经济地理学理论基础,考虑到同业影响因子,重新构建引力模型,并引入空间滞后因子,利用地理加权回归方法建立了估算区域间贸易流量的产业—空间统计模型,并在中国30 个省区投入产出表的基础上,以省区间农业、化工、通信电子3 个产业贸易流量的估算为例对上述方法进行了说明。结果表明：① 空间统计模型的应用可以显著提高区域间贸易流量的估算可靠性;② 随着空间权函数中带宽的缩小,贸易流量显得更加集中。因此,带宽在一定程度上反映了地理活动的空间集聚程度,不同行业应选取不同带宽;③ 不同行业有不同的同业影响机制和贸易特征,农业输出地以中部地区为主,目的地以沿海地区为主,具有一定的同业竞争关系,而化工、通信行业的产业流动主要发生在东部地区内部,具有很强的同业合作关系。  相似文献   

Spatial Variability of Soil Parameters of the van Genuchten Model at a Regional Scale   总被引：1，自引：0，他引：1       下载免费PDF全文

Yunqiang Wang  Ming'an Shao  Xiangwei Han  Zhipeng Liu 《洁净——土壤、空气、水》2015,43(2):271-278

  相似文献   

盐池县地质灾害遥感调查及空间分布特征分析          下载免费PDF全文

张晓东  刘湘南  赵志鹏  赵银鑫  马玉学  刘海燕 《水文地质工程地质》2017,(1):164-170

宁夏盐池县地处黄土高原区,地质灾害较为频繁。以SPOT6、RapidEye、无人机以及LandSat8 OLI等多源遥感数据为基础,通过研究遥感影像特征,建立地质灾害解译标志,共解译出滑坡125处、崩塌84处、泥石流19处、地面塌陷区3处。结合区域地理地质环境特征,总结了研究区地质灾害点的基本特征,并利用GIS技术对灾害点进行点密度分析,在此基础上划分了7个集中分布区,归纳了盐池县地质灾害点的空间分布特征及规律;同时,对研究区地层构造、植被、地形等因素与地质灾害点空间分布特征的相关性进行了讨论。研究结果表明:盐池县地质灾害点具有规模小,灾害轻;点密度整体南高北低,且南部聚集、北部分散;地层、植被、坡度、坡向等因素与地质灾害有着密切的联系。  相似文献   

新疆阿依托汉铜矿地质特征及找矿方向          下载免费PDF全文

陈孝聪  万生楠  李文杰  杨志鹏  杨秉飞 《地质找矿论丛》2017,32(2):227-235

阿依托汉矿区位于阿尔泰山区南缘的阿舍勒Cu-Au-Pb-Zn矿带,共发现5条铜矿体,铜矿体主要赋存于下-中泥盆统阿舍勒组第一岩性段的大理岩和变质凝灰岩中,少量产于石英斑岩脉中;与成矿有关的中泥盆世英云闪长岩和晚期岩脉提供了成矿热源并形成与矿化相关的矽卡岩化、硅化、绢云母化、绿帘石化等围岩蚀变;玛尔卡库里大断裂的次级断裂(F5韧脆性断裂)控制了铜矿体的储矿空间;成矿主要经过了早-中泥盆世(火山-沉积作用)、中泥盆世(岩浆侵入作用)和中-晚泥盆世(铜矿的主矿化阶段)多个阶段,是多种地质因素的耦合导致最终成矿。矿床体现了"层控-岩控-构控-时控"四位一体控矿的特点,不宜用单一的成矿模型予以描述定位,矿床类型属于热液交代-充填型铜矿床。文章在总结找矿标志的基础上,对下一步的找矿方向进行了探讨。  相似文献   

耕地资源数量变化与城镇化水平协同性关系研究——以合肥市为例     

余洋  梁宇生  张志鹏  田磊  何培雍  亓国涛 《国土资源导刊(湖南)》2017,14(1)

城镇化是衡量一个国家和地区工业化和现代化的重要标志,是实现区域社会经济增长、促进地区和谐发展的战略决策。随着城镇化水平的不断提升,合肥市耕地非农化速度过快、耕地资源数量大幅降低等现实问题凸显,导致城镇化发展与耕地保护之间的关系日趋复杂,进一步加剧了社会经济发展与耕地资源保护二者之间的矛盾。适时开展耕地资源数量变化与城镇化协同性关系研究,深入挖掘城镇化过程中耕地资源数量变化的内在规律,对于妥善处理经济发展与耕地保护、持续推动区域新型城镇化建设具有重要的理论价值和现实意义。  相似文献   

我国省域出口增加值的核算及其对产业结构的影响评估     

李方一  刘思佳  唐志鹏 《热带地理》2016,36(6):1026-1033

以 2010 年中国非竞争型区域间投入产出表为基础,对 30 个省区市的出口增加值进行核算,从全国和区域尺度分析其对产业结构的影响。结果显示：省域出口增加值对全国产业结构的影响存在显著差异,划分出资源消耗型、技术引领型、服务业促进型和出口起步型 4 类区域,前 3 类区域通过出口增加值分别提升了全国 GDP中资源密集型产业、技术密集型产业和服务业的比例;从出口增加值对本地产业结构的影响来看,欠发达地区出口增加值普遍有利于推动本地产业结构升级,发达地区出口增加值提升了资源密集型产业和技术密集型产业在地区 GDP 中的比例,但阻碍了服务业比例的提升,出口增加值结构需要进一步优化。最后提出促进和改善出口增加值的政策建议。  相似文献