首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   1篇
  完全免费   7篇
  地质学   8篇
  2012年   1篇
  2008年   1篇
  2007年   1篇
  2005年   1篇
  2004年   2篇
  2002年   1篇
  2000年   1篇
排序方式: 共有8条查询结果,搜索用时 156 毫秒
1
1.
东喜马拉雅构造结南迦巴瓦岩群的解体   总被引:16,自引:1,他引:15       下载免费PDF全文
通过对研究区南迦巴瓦岩群的大比例尺填图工作,根据南迦巴瓦岩群的原岩建造、变质程度的不同、变形样式的差异,将其解体为在区域上具有可填性3套岩石组合——直白岩组、派乡岩组和多雄拉混合岩,三者之间均以构造面接触。  相似文献
2.
南迦巴瓦构造结的楔入及其地质效应   总被引:8,自引:3,他引:5       下载免费PDF全文
南迦巴瓦构造结由其核 喜马拉雅构造单元和周边的冈底斯构造单元、雅鲁藏布构造单元组成。喜马拉雅构造单元为构造楔入体,两侧发育有右旋和左旋走滑断层系,构成南迦巴瓦楔入同迦巴瓦构造结的楔入作用,使雅鲁藏布缝合线横推错位,形成滇藏涡旋构造,并为雅鲁藏布大峡谷的形成奠定了基础。南迦巴瓦楔入构造的形成一印度板块连续的向北汇聚推挤作用发生反时针旋转有关,并可分为点碰撞(45Ma前)、碰撞楔入(45 ̄7Ma)和旋  相似文献
3.
野外地质填图和研究发现,东喜马拉雅构造结高喜马拉雅结晶岩系中有古老的花岗岩侵入,并在鲁霞地区圈定了9个花岗质侵入体。古老的花岗质岩石主要侵位于南迦巴瓦岩群直白岩组中,与南迦巴瓦岩群一起经历了麻粒岩相变质作用而形成花岗质片麻岩套。岩石类型有花岗闪长质片麻岩、黑云母花岗质片麻岩、闪长质片麻岩等。岩石化学研究表明这些花岗片麻岩套具“S”型特征,可能有深部幔源物质的加入。花岗岩形成深度在2~5km之间.侵位时代为552~525Ma,为新元古代晚期,属泛非期陆内演化阶段的产物。高喜马拉雅地区在元古宙末期形成了结晶基底。  相似文献
4.
The eastern Himalayan syntaxis in Namjagbarwa is a high-grade metamorphic terrain formed by the India-Eurasia collision and northward indentation of the Indian continent into Asia. Right- and left-lateral slip zones were formed by the indentation on the eastern and western boundaries of the syntaxis respectively. The Dongjug-Mainling fault zone is the main shear zone on the western boundary. This fault zone is a left-lateral slip belt with a large component of thrusting. The kinematics of the fault is consistent with the shortening within the syntaxis, and the slipping history along it represents the indenting process of the syntaxis. The Ar-Ar chronological study shows that the age of the early deformation in the Dongjug-Mainling fault zone ranges from 62 to 59 Ma. This evidences that the India-Eurasia collision occurred in the early Paleocene in the eastern Himalayan syntaxis.  相似文献
5.
雅鲁藏布蛇绿混杂带在南迦巴瓦峰地区呈弧形连续分布,主要岩石类型有石英岩和云母石英片岩、绿片岩、斜长角闪岩、变质辉长岩、变余辉绿岩等。主要造岩矿物中,角闪石属富镁的镁角闪石、镁闪石、韭闪角闪石、浅闪角闪石等;单斜辉石为富镁的类型,成分相当于透辉石;橄榄石为典型的镁橄榄石;斜长石在角闪岩类中为中长石,是变质成因的。利用地质温压计估算出的变质温压条件分别为:t=500~650℃,P=0.75~0.8GPa,相当于角闪岩相变质作用,发生在47~47Ma左右。晚期经历了低温、高压变质作用,形成高压型的多硅白云母,时代为27~20Ma,与该区结合带边界阿尼桥断层和米林.鲁朗断层发生强烈走滑有关。地壳加速隆升、剥蚀时期形成的多硅白云母为中、低压型。  相似文献
6.
7.
Many moraines formed between Daduka and Chibai in the Tsangpo River valley since Middle Pleistocene. A prominent set of lacustrine and alluvial terraces on the valley margin along both the Tsangpo and Nyang Rivers formed during Quaternary glacial epoch demonstrate lakes were created by damming of the river. Research was conducted on the geological environment, contained sediments, spatial distribution, timing, and formation and destruction of these paleolakes. The lacustrine sediments 14C (10537±268 aBP at Linzhi Brick and Tile Factory, 22510±580 aBP and 13925±204 aBP at Bengga, 21096±1466 aBP at Yusong) and a series of ESR (electron spin resonance) ages at Linzhi town and previous data by other experts, paleolakes persisted for 691~505 kaBP middle Pleistocene ice age, 75–40 kaBP the early stage of last glacier, 27–8 kaBP Last Glacier Maximum (LGM), existence time of lakes gradually shorten represents glacial scale and dam moraine supply potential gradually cut down, paleolakes and dam scale also gradually diminished. This article calculated the average lacustrine sedimentary rate of Gega paleolake in LGM was 12.5 mm/a, demonstrates Mount Namjagbarwa uplifted strongly at the same time, the sedimentary rate of Gega paleolake is more larger than that of enclosed lakes of plateau inland shows the climatic variation of Mount Namjagbarwa is more larger and plateau margin uplifted more quicker than plateau inland. This article analyzed formation and decay cause about the Zelunglung glacier on the west flank of Mount Namjagbarwa got into the Tsangpo River valley and blocked it for tectonic and climatic factors. There is a site of blocking the valley from Gega to Chibai. This article according to moraines and lacustrine sediments yielded paleolakes scale: the lowest lake base altitude 2850 m, the highest lake surface altitude 3585 m, 3240 m and 3180 m, area 2885 km2, 820 km2 and 810 km2, lake maximum depth of 735 m, 390 m and 330 m. We disclose the reason that previous experts discovered there were different age moraines dividing line of altitude 3180 m at the entrance of the Tsangpo Grand Canyon is dammed lake erosive decay under altitude 3180 m moraines in the last glacier era covering moraines in the early ice age of late Pleistocene, top 3180 m in the last glacier moraine remained because ancient dammed lakes didn’t erode it under 3180 m moraines in the early ice age of late Pleistocene exposed. The reason of the top elevation 3585 m moraines in the middle Pleistocene ice age likes that of altitude 3180 m. There were three times dammed lakes by glacier blocking the Tsangpo River during Quaternary glacial period. During other glacial and interglacial period the Zelunglung glacier often extended the valley but moraine supplemental speed of the dam was smaller than that of fluvial erosion and moraine movement, dam quickly disappeared and didn’t form stable lake.  相似文献
8.
东喜马拉雅南迦巴瓦峰地区地质构造十分复杂,对该区板块缝合带的空间位置问题,长期以来,一直认为沿雅鲁藏布江呈弧形展布。笔者以ETM+为主要信息源,以遥感与GIS为技术支撑,对南峰地区的断裂构造进行了详细的遥感解译分析,从构造统计分析的角度对断裂构造进行定量研究,从分维值及趋势值的空间分布及变化特征分析,认为缝合带的南东段、北段大致沿雅鲁藏布江展布,而北西段位于雅鲁藏布江的北西侧,沿东久-米林(断裂带)展布,这也与近几年来开展了1∶25万区域地质调查获得的新认识相一致。  相似文献
1
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号