“中央造山带”早古生代缝合带及构造分区概述   总被引：15，自引：2，他引：15  

陆松年于海峰  李怀坤陈志宏 王惠初＇张传林  相振群 《地质通报》2006,25(12):1368-1380

“中央造山带”是夹持于中国塔里木、华北和扬子克拉通之间的近东西向延展的（局部为北东向和北西向）显生宙造山系统。该造山带中包括了库地-喀拉塔什、红柳沟-肃北-北祁连、南阿尔金-滩间山、昆中、朱阳关-夏馆和商州-丹凤6条早古生代缝合带。被缝合带所围限的前寒武纪地质构造单元包括中阿尔金-祁连-金吉地块、柴达木地块、北秦岭地块和东、西昆仑2个变质地体。南秦岭原为扬子克拉通的北部边缘，但卷入了显生宙造山带，成为中央造山带的一部分。对上述6条早古生代缝合带和6个前寒武纪地质构造单元的特点进行了概略总结，并阐述了各地质构造单元中的构造地层系统和热-构造事件的年代格架。  相似文献   

青海南部金沙江缝合带二叠纪硅质岩地球化学特征及沉积环境   总被引：1，自引：1，他引：1  

段其发  王建雄  何龙清  赵小明  涂兵 《华南地质与矿产》2006,(3):24-30

青海省南部扎河地区金沙江缝合带中出露的通天河蛇绿混杂岩由不同时代、不同岩性的地层断片组成.对其中的二叠纪硅质岩进行地球化学研究后发现,该地区的硅质岩SiO2含量在71.56%～88.24%之间,Al/(Al Fe Mn)平均值为0.64,MnO/TiO2平均值为0.74,ΣREE平均为138.51×10-6,稀土元素配分曲线呈平坦型,δCe为0.97～1.49,平均为1.14,无明显异常;(La/Yb)N平均值为1.85,(La/Ce)N平均值为1.08,与已知大地构造背景的硅质岩地球化学特征对比,表明其形成环境为陆间洋盆环境.因此,金沙江带不能作为古特提斯域的主缝合带.  相似文献   

Structural Geochemical Study of the Yuxi Fold-Thrust Belt in the Southern North China Plate     

李文勇夏斌  李东旭 《中国地质大学学报(英文版)》2006,17(2):95-102

The gigantic fold-thrust fracture belt that ex-tends for 900 kmto the NWin the southern NorthChina plate strides across three provinces : Shaanxi ,Henan and Anhui .It is one of the most characteristicstructural deformations in the North China plate .Along this structural belt a series of i mportantcoalfields occur ( e . g. Pingdingshan, Queshan,Huainan) inthe southernmost edge of the North Chi-na coal-concentrating basin. Consequently ,this beltis not only of key value for research onthe…  相似文献   

布卡拉曼加拉贝氏牙形石动物群在西藏日土地区的发现及其意义     

纪占胜  姚建新  武桂春  刘贵忠 《地质通报》2006,(Z1)

布卡拉曼加拉贝氏牙形石动物群首次在西藏阿里日土县多玛区脱塔拉剖面的吞龙共巴组底部发现,主要由Rabeignathusbucaramangus,Sweetognathuswhitei,Sweetognathusironatus和Mesogondolellacf.bissilli组成,指示的地层时代为Artinskian中晚期—Kungurian早期。此前,该动物群仅发现于美国犹他州、堪萨斯州、哥伦比亚的布卡拉曼加、帕米尔东南部和中国滇西保山地区。该牙形石动物群的产出地点位于班公湖以北、龙木错以南的喀喇昆仑地层分区,跨越了班公湖-怒江断裂带北界,而这一动物群被认为是冈瓦纳北缘浅海区特有的浅水相类型,因此推测班公湖-怒江缝合带可能不是冈瓦纳大陆的北界。  相似文献   

黄淮海地区植被覆盖变化驱动力与驱动机制研究     

Du Zixuan  Chen Huailiang  Liu Zhongyang 《河南气象》2007,(3)

基于1982-2003年GIMMS NDVI遥感资料、气候资料和社会经济统计资料,利用主成分分析、逐步回归等方法,对黄淮海地区植被覆盖变化的驱动力和驱动机制进行了研究,从气候、社会经济两方面分析了区内6种植被类型区植被覆盖变化的驱动机制。结果发现,不同植被类型区,其驱动机制差别很大,但总体来说,区内各类植被类型区植被覆盖变化大都受到气候和人类活动的共同驱动,主要驱动力为气候因素,人类活动在局部区域能够产生较大作用,而大范围区域植被NDVI(归一化植被指数)的变化或改变,主要受气候变化的影响。在此基础上,分别建立了6种植被类型区年均NDVI变化驱动力模型。  相似文献   

A cost–benefit appraisal of coastal managed realignment policy     

R.K. Turner  D. Burgess  D. Hadley  E. Coombes  N. Jackson   《Global Environmental Change》2007,17(3-4):397-407

European coasts are coming under increasing threat as a result of climate change from erosion and flooding. While coastal defences such as sea walls have been constructed since Roman times to protect human settlements from the sea, it is now increasingly recognised that these defences are unsustainable. The security provided by ‘hard’ engineered defences has encouraged development on the coast, and the defences themselves have led to the loss of intertidal habitat and the natural protection it provides.An alternative to maintaining ‘hard’ defences (hold-the-line) to protect land from increasing sea levels is managed realignment, where the engineered defences are deliberately breached. By allowing the coastline to recede to a new line of defence further inland, intertidal habitat is created providing natural protection from flooding and erosion.The study evaluates the economic efficiency—using cost–benefit analysis—of various managed realignment scenarios compared to a strategy of holding-the-line within the Humber estuary in North-east England. The results of this analysis show that managed realignment can be more economically efficient than holding-the-line over a sufficiently long time period—generally greater than 25 years. Sensitivity analysis demonstrates that results are more sensitive to the amount and value of intertidal habitat generated than they are to the amount and value of carbon stored by this habitat. Cost–benefit analysis is viewed as one component of a wider policy appraisal process within integrated coastal management.  相似文献   

地下洞室超欠挖问题非线性有限元分析          下载免费PDF全文

刘建民  陈文涛  丁泰山 《探矿工程》2007,34(8):70-72

运用数值分析的方法,采用ANSYS10.0版有限元分析程序对洞室超欠挖进行三维模拟计算,分析了不同超挖位置、超挖深度、超挖数量等对洞室围岩稳定性的影响,得出了超欠挖部位应力集中数值解及塑性区产生的影响范围,为地下工程掘进施工和初期支护设计提供重要的参考依据。  相似文献   

贵州紫云扁平剖面早二叠世非筵有孔虫动物群   总被引：2，自引：0，他引：2  

董宝清刘家润  施贵军 《地层学杂志》2007,31(4):317-324,I0007

贵州紫云扁平剖面紫松阶上部一罗甸阶非筵有孔虫动物群由25属82种（含相似种、亚种而不含未定种）构成，其中7属（Cribrogenerina、Nodosaria、Glomospira、Tetrataxis、Palaeotextularia、Climacammina及Globival-vulina）的物种分异度最高，合计占总种数的71％；该动物群自紫松期开始发育，在隆林期类群构成发生显著变化并繁盛至罗甸早期，在罗甸中晚期明显衰落。研究剖面由下至上可划分为Cr拍rogPnP-nncelebrata-C．hemispaera间隔带、Glomospira-Nodosaria富集带（又可进而分为Geinitzina postcarbonica-Globivalvulina cyprica间隔亚带、Climacammina elegantula延限亚带）、Lasiodiscus-Eotuberitina间隔带。  相似文献   

Cenozoic volcanic rocks in the Belog Co area, Qiangtang, northern Tibet, China： Petrochemical evidence for partial melting of the mantle-crust transition zone     

LAI Shaocong QIN Jiangfeng LI Yongfeng LIU Xin 《中国地球化学学报》2007,26(3):305-311

Neogene volcanic rocks in the Belog Co area, Qiangtang, northern Tibet, are represented by a typical intermediate-basic and intermediate alkaline rock association, with latite-trachyte as the main rock type. The results of chemical analysis are: SiO2=52%–62%, Al2O3>15%, Na2O/K2O>1 and MgO<3.30%. In addition, the volcanic rocks are LREE-enriched with LREE/HREE=10–13, (La/Yb)N=15–19, and show a weak negative Eu anomaly with δEu=0.71–0.89. The close relationship between Mg# and SiO2 and the co-variation of the magmatophile elements and ultra-magmatophile elements such as La/Sm-La and Cr-Tb indicate that this association of volcanic rocks is the product of comagmatic fractional crystallization. The rock association type and lower Sm/Yb values (Sm/Yb=3.23–3.97) imply that this association of volcanic rocks should have originated from partial melting of spinel lherzolite in the lithospheric mantle. On the other hand, the weak negative Eu anomaly and relative depletion in Nb, Ta and Ti reflect the features of terrigenous magma. So the Neogene Belog Co alkaline volcanic rocks should be the result of partial melting of the special crust-mantle transition zone on the Qinghai-Tibet Plateau.  相似文献   

龙永聚煤盆地构造演化与富煤带展布的相关性分析     

何仲秋 《中国煤田地质》2007,19(4):5-9

通过龙永聚煤盆地构造演化及富煤带赋存层段机理分析,发现聚煤盆地构造演化与富煤带展布有一定的相关性,主要表现在一定时期、一定空间、一定样式的构造与一定层段的富煤带在走向、倾向上,具有一定的相关性,即一定的富煤带产生在一定的滑覆、推覆构造及其组合中。龙永煤田西部主要产生印支期的滑覆断层,应寻找走向上的富煤带;龙永煤田东部主要产生燕山期的推覆断层,应寻找倾向上的富煤带;龙永煤田中部主要产生印支期及燕山期的组合滑脱断层,应寻找上推下留型、上滑下留型、滑褶集中型的走向、倾向的富煤带。此项研究为龙永煤田进一步寻找富煤带指明了方向,同类型的勘探区可以参考。  相似文献