西藏地质旅游资源概况及开发建议     

段丽萍 《地质通报》2006,(Z1)

西藏地区孕育了如地貌、水体、地质构造、地层剖面和地质灾害遗迹等种类繁多的地质遗迹资源,使得西藏发展地质旅游成为可能。在概述西藏地质旅游资源的基础上,论述了开发西藏地质旅游资源对西藏社会经济可持续发展、改善西藏投资环境和提高招商引资环境容量的重要意义,提出了在开发过程中应遵循“在保护中开发和在开发中保护”的总体原则及几点相关建议。  相似文献   

金顶铅锌矿床地质特征及成因探讨   总被引：7，自引：0，他引：7  

付修根  庞艳春 《世界地质》2004,23(3):238-244

金顶铅锌矿床以陆相碎屑岩为主岩，明显区别于以海相碳酸盐岩为主岩的MVT矿床；其成矿背景、矿体产状及ωPb／ωZn都与SST铅锌矿床有较大差异；金顶铅锌矿床与SEDEX矿床相比，在矿体产状、金属—矿物分带、矿体上下盘特征以及接触界线上均存在一定差异。矿床特征的研究发现，金顶铅锌矿床上有盖层，下有遮档层，中间为孔隙度、渗透率较好的储集层，这一岩套组合类似于油气的生成，而穹窿、F2断层形成的构造空间则为成矿流体的贮集、沉淀和成矿提供了条件。  相似文献   

黑龙江省虎林市幅重磁场特征及其地质解释   总被引：1，自引：0，他引：1  

林泽付  薛进  杨恕  吴东国 《世界地质》2004,23(4):397-401

以区域地质资料和物性资料为依据，对黑龙江省虎林市幅重磁场特征进行了综合分析。根据航磁△T异常以及布格异常平面等值线展布特点，对该区的杂乱磁场区、线性磁场区和平稳磁场区进行了相关的地质解释，描述了30条断裂构造带及其重力场特征；结合重力异常和航磁异常等综合资料，按结晶基底起伏形态，将虎林盆地划分为4个隆起、3个凹陷共7个构造单元。  相似文献   

Crustal structure beneath the Songpan——Garze orogenic belt     

王椿镛  韩渭宾  吴建平  楼海  白志明 《地震学报(英文版)》2003,(3)

AbstractThe Benzilan-Tangke deep seismic sounding profile in the western Sichuan region passes through the Song-pan-Garze orogenic belt with trend of NNE.Based on the travel times and the related amplitudes of phases in therecord sections,the 2-D P-wave crustal structure was ascertained in this paper. The velocity structure has quitestrong lateral variation along the profile.The crust is divided into 5 layers,where the first,second and third layerbelong to the upper crust,the forth and fifth layer belong to the lower crust.The low velocity anomaly zone gener-ally exists in the central part of the upper crust on the profile,and it integrates into the overlying low velocitybasement in the area to the north of Ma’erkang.The crustal structure in the section can be divided into 4 parts:inthe south of Garze-Litang fault,between Garze-Litang fault and Xiashuihe fault,between Xianshuihe fault andLongriba fault and in the north of Longriba fault,which are basically coincided with the regional tectonics division  相似文献   

Re-discussion　on　the　Jiaochang　Arcuate　Structure,　Sichuan　Province,　and　the　Seismogenic　Structure　for　Diexi　Earthquake　in　1933     

HuangZuzhi TangRongchang LiuShengli 《中国地震研究》2003,17(1):51-62

The Jiaochang arcuate structure is one of the numerous arcuate structural belts in Sichuan. The present paper gives a further argument about the characteristics of that arcuate structure and the new activity of the Songpinggou fault and affirms that the Songpinggou fault is an active fault in the Holocene epoch. The Diexi M7.5 earthquake took place in 1933 on the west wing of that arcuate structure, near the apex of the arc. Many authors have given quite different opinions about the genetic structure of that earthquake. The authors have made on-the-spot investigations time and again over recent years. Besides this, the authors have also further studied the shape of intensity contour lines, the distribution characteristics of ground surface seismic hazards, the left-lateral dislocation of buildings along the Songpinggou fault, the NWtrending ground fissures that developed on the ground surface after earthquake, and so on. On this basis, it is still considered that the seismogenic fault of the 1933 Diexi M7.5 earthquake was the Songpinggou fault on the west wing of the Jiaochang arcuate structure.  相似文献   

河南洛宁太华岩群斜长角闪岩的锆石^207Pb／^206Pb和角闪石^40Ar／^39Ar年龄   总被引：2，自引：0，他引：2  

倪志耀  王仁民  童英  杨淳  戴潼谟 《地质论评》2003,49(4):361-366

运用单颗粒锆石逐层蒸发法和角闪石40Ar/39Ar阶段加热法研究了河南洛宁太华岩群斜长角闪岩的同位素年龄.获得锆石207Pb/206Pb年龄为2675±2 Ma,角闪石40Ar/39Ar坪年龄和等时线年龄分别为2372.98±47.46 Ma和2349.10±46.98 Ma.锆石207Pb/206Pb年龄代表了斜长角闪岩原岩的形成时代,而角闪石40Ar/39Ar年龄则为其变质时代,与Sm-Nd等时线年龄(2351±103Ma)相一致.上述年龄数据表明河南洛宁地区太华岩群形成于新太古代,在古元古代遭受过一次角闪岩相变质作用.  相似文献   

川滇黔桂地区志留纪构造－岩相古地理   总被引：19，自引：5，他引：19       下载免费PDF全文

万方  许效松 《古地理学报》2003,5(2):180-186

晚奥陶世与早志留世之间的都匀运动，使滇中古隆起与黔中古隆起成为一整体隆起带（习惯上称黔中古陆），把滇东南和黔南与滇东北-黔北-川南分隔为南、北两个不同的构造沉积域。南侧的曲靖一带出露下、中寒武统，其上分别与中、上志留统和下泥盆统呈假整合，其间缺失奥陶纪和早志留世的沉积物。北侧的禄劝－武定一带，下古生界的沉积序列与之相反，有完整的奥陶纪沉积组合，上与泥盆系假整合，其间无志留纪的沉积。这表明黔中古陆两侧的沉积域各为独立的系统。中晚志留世，黔中古隆起南侧应归属于上扬子与滇黔桂地块前陆挠曲盆地的一部分，由曲靖向北东经赫章哑都-贵阳南转向湘西，向南则与云南的绿春海相连，黔中古隆起北侧的沉积域则为上扬子前陆（川南-黔北）盆地的边缘相。  相似文献   

Carbonate Sequence Stratigraphy of a Back-Arc Basin： A Case Study of the Qom Formation in the Kashan Area, Central Iran          下载免费PDF全文

XU Guoqiang ZHANG Shaonan LI Zhongdong SONG Lailiang LIU Huimin 《《地质学报》英文版》2007,81(3):488-500

The Qom Formation comprises Oligo-Miocene deposits from a marine succession distributed in the Central Basin of Iran. It is composed of five members designated as A-F. Little previous work exists on the sequence stratigraphy. Based on an integrated study of sequence stratigraphy with outcrop data, wells and regional seismic profiles, the Qom Formation is interpreted as a carbonate succession deposited in a mid-Tertiary back-arc basin. There are two second-order sequences (designated as SS1 and SS2) and five third-order sequences (designated as S1-S5). Five distinct systems tracts including transgressive, highstand, forced regressive, slope margin and lowstand have been recognized. The relationship between the sequences and lithologic sub-units has been collated and defined (S1 to S5 individually corresponding to A-C1, C2-C4, D-E, the lower and upper portions of F); a relative sea level change curve and the sequence stratigraphic framework have been established and described in detail. The coincidence of relative sea level change between that of the determined back-arc basin and the world indicates that the sedimentary cycles of the Qom Formation are mainly controlled by eustatic cycles. The variable combination of the systems tracts and special tectonic-depositional setting causally underpin multiple sequence stratigraphic framework styles seen in the carbonates of the back-arc basin revealing: (1) a continental margin basin that developed some form of barrier, characterized by the development of multiple cycles of carbonate-evaporites; (2) a flat carbonate ramp, which occurred on the southern shelf formed by the lack of clastic supply from nearby magmatic islands plus mixed siliciclastics and carbonates that occurred on the northern shelf due to a sufficient clastics supply from the land; and (3) a forced regressive stratigraphic stacking pattern that occured on the southern shelf and in basin lows due to the uplifting of the southern shelf. Thick and widespread aggradational framework limestone usually occurs in the initial sequences (S1 and S3) of the supersequence, which led to preferential oil reservoir deposition but a lack of source and cap rocks, whereas the retrogradational and progradational framework limestone usually occurs in the later sequences (S2 and S4-S5) of the supersequence, which results in two perfect sets of source, reservoir and cap rock assemblies, so that the limestone in sub-member C2-C4 and the F-Member can be predicted as important objects for oil exploration.  相似文献   

Large-scale Tazhong Ordovician Reef-flat Oil-Gas Field in the Tarim Basin of China   总被引：5，自引：5，他引：0  

ZHOU Xinyuan  WANG Zhaoming  YANG Haijun  ZHANG Lijuan  HAN Jianf  WANG Zhenyu 《《地质学报》英文版》2009,83(1):179-188

The Tazhong reef-flat oil-gas field is the first large-scale Ordovician organic reef type oil-gas field found in China. Its organic reefs were developed in the early Late Ordovician Lianglitag Formation, and are the first large reefs of the coral-stromatoporoid hermatypic community found in China. The organic reefs and platform-margin grain banks constitute a reef-flat complex, mainly consisting of biolithites and grainstones. The biolithites can be classified into the framestone, bafflestone, bindstone etc. The main body of the complex lies around the wells from Tazhong-24 to Tazhong-82, trending northwest, with the thickness from 100 to 300 m, length about 220 km and width 5-10 km. It is a reef-flat lithologic hydrocarbon reservoir, with a very complex hydrocarbon distribution: being a gas condensate reservoir as a whole with local oil reservoirs. The hydrocarbon distribution is controlled by the reef complex, generally located in the upper 100-200 m part of the complex, and largely in a banded shape along the complex. On the profile, the reservoir shows a stratified feature, with an altitude difference of almost 2200 m from southeast to northwest. The petroleum accumulation is controlled by karst reservoir beds and the northeast strike-slip fault belt. The total geologic reserves had reached 297.667 Mt by 2007.  相似文献   

Structure,Orientation and Finite Element Analysis of the Tail Club of Mamenchisaurus hochuanensis   总被引：2，自引：1，他引：1  

XING Lid  YE Yong  SHU Chunkang  PENG Guangzhao  YOU Hailu 《《地质学报》英文版》2009,83(6):1031-1040

Abstract: The structure and orientation of the posterior extremity (tail club) of the caudal vertebrae of Mamenchisaurus hochuanensis Young and Chao, 1972 from the Upper Jurassic Shangshaximiao Formation has been analyzed to determine the tail club function using Finite Element Analysis. Of the four caudal vertebrae composing the tail club, the second largest (C"1") was probably the most proximal, and is fixed with the preceding sequence of the caudal vertebrae, whereas the smallest (C"4") is free and forms the termination of the tail club. Our analysis also suggests that the tail club is more efficient in lateral swinging rather than up-and-down motion, and that the best region for the tail club to impact is at the spine of the largest of the four caudals (C"2"), with a maximum load for impact at about 450 N. The tail club of Mamenchisaurus hochuanensis probably also had limitations as a defense weapon and was more possibly a sensory organ to improve nerve conduction velocity to enhance the capacity for sensory perception of its surroundings.  相似文献