羌塘中央隆起带深部结构特征研究及其意义
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摘要
羌塘含油气盆地是我国境内最大的中新生代海相沉积盆地.羌塘地体内的中央隆起将盆地分为南北两个盆地.中央隆起带构造属性认识存在两种截然不同的分歧,一是伸展环境下形成,整个羌塘盆地有着同一的基底.而另一认识其是一古特提斯缝合带,其两侧盆地具有不同的演化机制.调查羌塘中央隆起的深部结构特征及其与南北两侧的盆地间的构造关系是认识羌塘盆地基底性质及其油气远景之关键科学问题.尽管羌塘地体在青藏高原形成演化过程中遭到了强烈改造,但在收集并分析已有地球物理资料基础上认为其深部结构仍有可能被完整保存.因此,利用密集宽频带流动台网观测,获取其深部结构,进而研究其与两侧盆地关系,是当前羌塘含油气盆地研究之重要突破口,同时该项研究符合我国当前国家油气资源战略评估政策.
The Qiangtang basin bearing oil and gas is the largest Mesozoic-and Cenozoic marine sediment basin in China. The central uplift belt divides the Qiangtang basin into two sub-basins. So far, there are two contrary arguments for the development of the central uplift belts within Qiangtang terrane. One suggests that it formed under extension setting of the Qiangtang terrane in Carboniferous, which has the same basement with the southern Qiangtang basin and Northern Qiangtang basin. The other is that the central uplift belt was a paleotethyan suture, on its both side are present different evolution processes for the southern Qiangtang basin and norhtern Qiangtang basin. Some information from existing geophysical evidence show that the deep structure of the central uplift belt had been possible to be totally presered. To further accurately evaluate the perspective of the oil-bearing Qiangtang basin, it is very essential to survey the deep structure of the central uplift belt by broadband seismic observations. Also, the study well accords with currently macroscopical development of China.
The Qiangtang basin bearing oil and gas is the largest Mesozoic-and Cenozoic marine sediment basin in China. The central uplift belt divides the Qiangtang basin into two sub-basins. So far, there are two contrary arguments for the development of the central uplift belts within Qiangtang terrane. One suggests that it formed under extension setting of the Qiangtang terrane in Carboniferous, which has the same basement with the southern Qiangtang basin and Northern Qiangtang basin. The other is that the central uplift belt was a paleotethyan suture, on its both side are present different evolution processes for the southern Qiangtang basin and norhtern Qiangtang basin. Some information from existing geophysical evidence show that the deep structure of the central uplift belt had been possible to be totally presered. To further accurately evaluate the perspective of the oil-bearing Qiangtang basin, it is very essential to survey the deep structure of the central uplift belt by broadband seismic observations. Also, the study well accords with currently macroscopical development of China.
引文
[1] 王成善,伊海生,李勇,等.西藏羌塘盆地地质演化与油气远景评价[M].北京:地质出版社,2001． Wang C S, Yin H S, Li Y, et al. Geological evolution of Qiangtang Basin in Tibet and its oil and gas exploration prospects[M]. Beijing:Geological Publication House,2001．
[2] 赵政璋,李永铁,郭祖军,等.青藏高原油气勘探前景[J].勘探家,1997,2(3) :14-16． Zhao Z Z, Li Y Y, Guo Z J, et al. Oil and gas exploration prospects for tibet plateau [J]. Petroleum Explorationist. 1997,2(3) : 14-16．
[3] 黄继钧.藏北羌塘盆地构造特征及演化[J].中国区域地质,2001,20(2) :178-186． Huang J J. Tectonic characterises and evolution of the Qiangtang basin[J]. Regional Geology of China. 2001,20(2) : 178-186．
[4] 吴瑞忠,胡承祖,王成善.藏北羌塘地区地层系统[M].见:青藏高原地质文集(9) ,北京:地质出版社,1985,1-32． Wu R Z, Hu C Z, Wang C S. Stratum system of Qiangtang terrane, Northern Tibet [M]. See: Geological Corpus of Tibetan Plateau (9) , Beijing: Geological Publication House, 1985,1-32．
[5] 王成善,胡承祖,吴瑞忠,等.西藏北部查桑-茶布裂谷的发现及其地质意义[J].成都地质学院学报,1987,14(2) :33-46． Wang C S, Hu C Z, Wu R Z, et al. Significance of the discovery of Chasang-Chabu rift in Northern Xizhang (Tibet) [J]. Journal of Chengdu College of Geology, 1987, 14(2) : 33-46．
[6] Sengor A. M. C. Plate tectonics and orogenic research after 25 years; A Tethyan perspective[J]. Earth Sci. Rev. , 1990, 27: 1-201．
[7] Kapp P., Yin A., Manning C. E. et al. Blueschist-bearing metamorphic core complexes in Qiangtang block reveal deep crustal structure of northern Tbiet[J]. Gology, 2000, 28(1) : 19-22．
[8] 尹福光.羌塘盆地中央隆起性质与成因[J].大地构造与成矿,2003,27(2) :143-146． Yin F G. Nature and origin of the central uplift in the Qiangtang basin[J]. Geotectonica et Metallogenia, 2003, 27(2) : 143-146．
[9] 李才,龙木错-双湖-澜沧江板块缝合带与石炭-二叠纪冈瓦纳北界[J].长春地质学院学报,1987,17(2) :156-166． Li C . The Longmucuo-Shuanghu-Lanchangjiang plate suture and the north boundary of distribution of Gondwana facies Permian-Carboniferous system in northern Xizang, China[J]. Journal of Changchun University of Earth Science, 1987, 17 (2) : 155-166．
[10] 李才,翟庆国,董永胜,等.青藏高原羌塘中部榴辉岩的发现及其意义[J].科学通报,2006,51(1) :70-74． Li C, Zhai Q G, Dong Y S, et al. The discovery of t he eclogite in Qiangtang area, Tibet [J]. Chinese Science Bulletin, 2006 ,51(1) :70274．
[11] 李才,翟庆国,陈文,等.青藏高原龙木错-双湖板块缝合带闭合的年代学证据--来自果干加年山蛇绿岩与流纹岩Ar-Ar和SHRIMP年龄制约[J].岩石学报,2007,23(5) :911-918． Li C, Zhai Q G,Chen W, et al. Geochronology evidence of the closure of Longmu CoShuanghu suture, Qinghai-Tibet plateau: Ar-Ar and zircon SHRIMP geochronology from ophiolite and rhyolite in Guoganjianian[J]. Acta Petroligca Sinica, 2007,23(5) :911-918．
[12] Hening A. EurPetrographic and Geologie Von Sudwest Tibet [M]. In: Hedin S et. Southern Tibet 5． Stockholm, 1915．
[13] 李才,程立人,胡克,等.西藏龙木错-双湖古特提斯缝合带研究[M].北京:地质出版社,1995． Li C, Cheng L R, Hu K, et al. Study on the paleo-Tethys suture zone of Lungmu Co-Shuanghu, Tibet[M]. Beijing: Geological Publishing House, 1995．
[14] 李才,王天武,杨德明,杨日红.西藏羌塘中央隆起区物质组成与构造演化[J].长春科技大学学报,2001,31(1) :25-31． Li C, Wang T W, Yang D M, et al. The lithological composition and tectonic evolution of Qiangtang central uplift region, Tibet [J]. Journal of Changchun University of Science and Technology, 2001,31(1) :25-31．
[15] 胡克,李才,程立人,等.西藏冈玛错-双湖蓝片岩带及其构造意义[J].长春地质学院学报,1995,23(3) :268-274． Hu K, LI C, Cheng L R, et al. Gangmacuo-Shuanghu blueschist belt in central Qiangtang area of Tibet and it s geological significance[J]. Journal of Changchun University of Earth Sciences, 1995, 23(3) :268-274．
[16] 邓万明,尹集祥,呙中平.羌塘茶布-双湖地区基性超基性岩、火山岩研究[J].中国科学:D辑,1996,26(4) :296-301． Deng W M, Yin J X, Wo Z P. Study on basic-ultrabasic and volcanic rocks of Chabu Shuanghu in Qiangtang[J]. Science in China :Series D,1996,26(4) :2962301．
[17] 鲍佩声,肖序常,王军,等.西藏中北部双湖地区蓝片岩带及其构造涵义[J].地质学报,1999,73(4) :302-314Bao P S, Xiao X C, Wang J, et al. Blueschist belt of Shuanghu area in cent ralnort hern Xizang (Tibet) and it s tectonic implications [J]. Acta Geologica Sinica, 1999, 73 (4) :302-314．
[18] 邓希光,丁林,刘小汉,等.藏北羌塘中部冈玛日-桃形错蓝片岩的发现[J].地质科学,2000,35(2) :227-232． Deng X G, Ding L, Liu X H, et al. Discovery of blueschist s in Gangmar-Taoxing Co area, cent ral Qiangtang, northern Tibet [J]. Scientia Geologica Sinica, 2000, 35 (2) : 227-232．
[19] 邓希光,丁林,刘小汉,等.青藏高原羌塘中部蓝片岩的地球化学特征及其构造意义[J].岩石学报,2002,18(4) :517-525． Deng X G, Ding L, Liu X H, et al. Geochemical characteristics of t he blueshist s and it s tectonic significance in cent ral Qiangtang area , Tibet [J]. Acta PetrologicaSinica,2002,18(4) :517-525．
[20] 李春昱.试谈板块构造[J].西北地质科技情报,1973,第一期(增刊):1-26． Li C Y. Discourse of Plate tectonics [J]. Northwestern Geological Information, 1973,1(Supp.):1-26．
[21] Dobretsov N L. Blueshists and eclogites: a possible plate tectonic mechanism for their emplacement from the upper mantle. Tectonophysics[J]. 1991,186:253-268．
[22] 任纪舜 主编.中国及邻区大地构造图[M].北京:中国地质出版社,1997． Ren J S. The tectonic map of t he Peopleps Republic of China and adjacent area [M]. Beijing: Geological Publishing House, 1997．
[23] 常承法,潘裕生,郑锡澜.青藏高原地质构造,北京:科学出版社,1982． Chang C F, Pan Y S, Zheng X L, et al. The geological tectonics of Qinghai-Xizang (Tibet) plateau. Beijing: Science Press, 1982．
[24] 尹安.喜马拉雅-青藏高原造山带地质演化-显生宙亚洲大陆生长.地球学报,2001,22(3) :193-230． Yin A. Geologic evolution of the Himalayan-Tibtan orogen-Phanerozoic growth of Aisa continetal. Acta Geoscientia Sinica (in Chinese) , 2001, 22(3) : 193-230．
[25] 郭新峰,张元丑,程庆云,等.青藏高原亚东-格尔木地学断面岩石圈电性研究[J].中国地质科学院院报,1990,21:191-202． Guo X F, Zhang Y C, Cheng Q Y, et al. Magnetotelluric studies along Yadong-Golmud geosciences transect in Qinghai-Xizang plateau[J]. Bulletin of The Chinese Academy of Geological Sciences (in Chinese), 1990, 21:191-202．
[26] 秦国卿,陈九辉,刘大建等.昆仑山脉河喀喇昆仑山脉地区的地壳上地幔电性结构特征[J].地球物理学报,1994,37(2) :193-199． Qin G Q, Chen J H, LIU D J, et al. The characteristics of the electrical structure of the crust and upper mantle in the the region of the Kunlun and the Karakorum Mountains[J]. Acta Geophysica Sinica,1994,37(2) : 193-199．
[27] 孔祥儒,王谦身,熊绍柏.青藏高原西部综合地球物理与岩石圈结构的研究[J].中国科学(D辑),1996,26(4) :308-315． Kong X R, Wang Q S, Xiong S B. Comprehensive geophysics and lithospheric st ructure in t he western Xizang (Tibet) plateau [J]. Scince in China:Series D, 1996 , 26 (4) :308-315．
[28] 张胜业,魏胜,王家映,等.西藏羌塘盆地大地电磁测深研究[J].地球科学,1996,21(1) :198-202． Zhang S Y, Wei S, Wang J Y, et al . Magnetotelluric sounding in the Qiangtang basin of Xizang (Tibet) [J]. Earth Science, 1996,21(2) : 1982202．
[29] 鲁兵,徐可强,刘池阳.藏北羌塘地区的地壳电性结构及其意义[J].地学前缘,2003,10(Sup.):153-159． Lu B, Xu KQ, Liu C Y, Electrical structure of crust in the qiangtang region , northern Tibet and its geological significance[J]. Earth Science Frontiers (China University of geosciences, Beijing), 2003． 10 (Sup.): 153-159．
[30] 魏文博,金胜,叶高峰,等.藏北高原地壳及上地幔导电性结构-超宽频带大地电磁测深研究结果[J].地球物理学报,2006,49(4) :1215-1225． Wei W B, Jin S, Ye G F, et al. Conductivity structure of crust and upper mantle beneath the northern Tibetan Plateau: Results of super-wideband magnetotelluric sounding [J]. Chinese J. Geophys. 2006,49(4) : 1215-1225．
[31] Zhao W, Mechie J, Brown, L D, et al. Crustal structure of the central Tibet as derived from project INDEPTH wideangle seismic data [J]. Geophys. J. Int. 2001,145:486-498．
[32] Haines S, Klemperer S L, Brown L, et al. Crustal thickening processes in central Tibet: implications of INDEPTH Ⅲ seismic data[J]. Tectonics 2003, 22:1-18．
[33] Ross A R, Brown L D, Pananont P. et al. Deep reflection surveying in central Tibet: lower-crustal layering and crustal flow[J]. Geophys. J. Int. , 2004, 156:115-128．
[34] 卢占武.青藏高原羌塘盆地岩石圈结构及其对油气远景的影响[博士论文].北京:中国地质科学院,2006． Lu Z W, Lithosphere structure of the Qiangtang basin, Qinghai-Tibetan plateau and its influence on petroleum prospcet[D]. Beijing: Chinese Academy Geological Sciences, 2006．
[35] 卢占武.青藏高原羌塘地体地壳精细结构横剖面-贯穿南北的地震反射探测试验研究[博士后出站报告].中国地质科学院,2008． 12． Lu Z W. The crustal fine structure of the Qiangtang terrance in the Tibetan plateau-Study on the N-S trending seismic reflection profile [Post Ph. D. thesis]. Beijing: Chinese Academy Geological Sciences, 2008． 12．
[36] Wittlinger G, Vergne J, Tapponnier P, et al. Teleseismic imaging of subducting lithosphere and Moho offsets beneath western Tibet. Earth and Planetary Sci. Lett., 2004,221: 117-130．
[37] Wittlinger G, Masson F, Poupinet G, et al. Seismic tomography of northern Tibet and Kunlun: Evidence for crustal blocks and mantle velocity contrasts[J]. Earth and Planetary Science letters, 1996, 139:263-279．
[38] Tilmann F, Ni J. INDEPTH Ⅲ Seismic Team, Seismic imaging of the downwelling Indianlithosphere beneath central Tibet[J]. Science, 2003,300:1424-1427．
[39] He R, Zhao D, Zheng H, et al. Teleseismic P-wave tomography under the central Tibet Plateau (Abstract) , EOS,AGU-2006WPGM, 2006,T12B-04．
[40] Zhao D, Hasegawa A, Horiuchi S. Tomographic imaging of P and S wave velocity structure beneath northeastern Japan [J]. J. Geophys. Res. 1992,97:19909-19928．
[41] Zhao D, Hasegawa A, Kanamori H. Deep structure of Japan subduction zone as derived from local, regional and teleseismic events[J]. J. Geophys. Res. 1994 , 99: 22313-22329．
[42] Zhao D. New advances of seismic tomography and its applications to subduction zones and earthquake fault zones: a review[J]. The Island Ar, 2001c 10, 68-84．
[43] 贺日政,赵大鹏,高锐,等.西昆仑造山带下岩石圈地幔速度结构[J].地球物理学报,2006,49(3) :778-787． He R Z, Zhao D P, Gao R, et al. Teleseismic P-wave tomography of lithospheric mantle beneath west Kunlun orogenic belts[J]. Chinese J. Geophys. (in Chinese), 2006, 49(3) :778-787．
[44] 郑洪伟.青藏高原地壳上地幔三维速度结构及其地球动力学意义[博士论文].北京:中国地质科学院,2006． Zheng H W. 3-D velocity structure of the crust and upper mantle in Tibet and its geodynamic effect [Ph. D. thesis]. Beijing:Chinese Academy Geological Sciences,2006．
[45] 郑洪伟,李廷栋,高锐,等.印度板块岩石圈地幔向北俯冲到羌塘地体之下的远震P波层析成像证据[J].地球物理学报,2007,50(5) :1418-1426． Zheng H W, Li T D, Gao R, et al. , Teleseismic P-wave tomography evidence for the Indian lithospheric mantle subducting northward beneath the Qiangtang terrane [J]. Chinese Journal of Geophysics,2007 ,50(5) : 1418-1426．
[46] Tian X B, Wu Q J, Zhang Z J, et al. Joint imaging by teleseismic converted and multiple waves and its applicaton in the IND EPTH-Ⅲ passive seismic arry [J]. Geophysical Research Letters, 2005, 32(L21315) , doi: 10． 1029/2005GL023686．
[47] Willett S D, Beaumont C. Subduction of Asian lithospheric mantle beneath Tibet inferred from models of continental collision[J]. Nature, 1994,369:642-645．
[48] 滕吉文,张中杰,万志超,等.羌塘盆地及周边地带地球物理场与油气深部构造背景初探[J].地球物理学进展,1996,11(1) :12-27． Teng J W, Zhang Z J, Wan Z C, et al. The preliminary study of geophysical field and deep structural background of oil and gas for Qiangtang Basin and its neighboring regions [J]. Geophysical Development ,1996 ,11(1) :15216．
[49] 贺日政.青藏高原近南北向裂谷的岩石圈结构及其动力学过程[博士论文].北京:中国地质科学院,2003． He R Z. Lithospheric Structure of near north-south striking rifts in tibet plateau and its geodynamical process [Ph. D. thesis]. Beijing: Chinese Academy Geological Sciences, 2003．
[50] 刘池阳,杨兴科,魏永佩,等.藏北羌塘盆地西部查桑地区结构及结构特征[J].地质论评,2002,48(6) :593-602． Liu C Y, Yang X K, Wei Y P, et al. Structure and tectonic feature of Chasang area in west part of Qiangtang basin, north part of Tibet[J]. Geologcial review, 2002 ,48(6) :593-602．
[51] 王喜臣,贾建秀,徐宝慈.羌塘拗陷石油地质走廊剖面重磁异常处理模拟及地质解释[J].吉林大学学报(地球科学版),2008,38(4) :685-691． Wang X C, Jia J X, XU B C. Gravity/Magnetic modeling and geological explanation in Qiangtang Basin geologic aisle [J]. Journal of Jilin University (Earth Science Edition), 2008, 38 (4) :685-691．
[52] 苑守成,于国明,田黔宁.青藏高原羌塘盆地重磁剖面异常与基底构造特征[J].地质通报,2007,26(6) :703-709． Yuan S C, Yu G M, Tian Q N. Gravity and magnetic anomaly profiles and characteristics of basement structure in the Qiangtang basin[J]. Qinghai-Tibet Plateau, Geological Bulletin of China, 2007, 26(6) :703-709．
[53] 田黔宁,耿涛,杨汇群,等.青藏高原西部重力异常剖面拟合及其地质解释[J].地质通报,2008,27(12) :2108-2116． Tian Q N, Geng T, Yang H Q, et al. Gravity anomalies forward fitting and geological explanation in the western Qinghai-Tibet Plateau [J]. Geologcial Bulletin of China, 2008,27(12) :2108-2116．
[2] 赵政璋,李永铁,郭祖军,等.青藏高原油气勘探前景[J].勘探家,1997,2(3) :14-16． Zhao Z Z, Li Y Y, Guo Z J, et al. Oil and gas exploration prospects for tibet plateau [J]. Petroleum Explorationist. 1997,2(3) : 14-16．
[3] 黄继钧.藏北羌塘盆地构造特征及演化[J].中国区域地质,2001,20(2) :178-186． Huang J J. Tectonic characterises and evolution of the Qiangtang basin[J]. Regional Geology of China. 2001,20(2) : 178-186．
[4] 吴瑞忠,胡承祖,王成善.藏北羌塘地区地层系统[M].见:青藏高原地质文集(9) ,北京:地质出版社,1985,1-32． Wu R Z, Hu C Z, Wang C S. Stratum system of Qiangtang terrane, Northern Tibet [M]. See: Geological Corpus of Tibetan Plateau (9) , Beijing: Geological Publication House, 1985,1-32．
[5] 王成善,胡承祖,吴瑞忠,等.西藏北部查桑-茶布裂谷的发现及其地质意义[J].成都地质学院学报,1987,14(2) :33-46． Wang C S, Hu C Z, Wu R Z, et al. Significance of the discovery of Chasang-Chabu rift in Northern Xizhang (Tibet) [J]. Journal of Chengdu College of Geology, 1987, 14(2) : 33-46．
[6] Sengor A. M. C. Plate tectonics and orogenic research after 25 years; A Tethyan perspective[J]. Earth Sci. Rev. , 1990, 27: 1-201．
[7] Kapp P., Yin A., Manning C. E. et al. Blueschist-bearing metamorphic core complexes in Qiangtang block reveal deep crustal structure of northern Tbiet[J]. Gology, 2000, 28(1) : 19-22．
[8] 尹福光.羌塘盆地中央隆起性质与成因[J].大地构造与成矿,2003,27(2) :143-146． Yin F G. Nature and origin of the central uplift in the Qiangtang basin[J]. Geotectonica et Metallogenia, 2003, 27(2) : 143-146．
[9] 李才,龙木错-双湖-澜沧江板块缝合带与石炭-二叠纪冈瓦纳北界[J].长春地质学院学报,1987,17(2) :156-166． Li C . The Longmucuo-Shuanghu-Lanchangjiang plate suture and the north boundary of distribution of Gondwana facies Permian-Carboniferous system in northern Xizang, China[J]. Journal of Changchun University of Earth Science, 1987, 17 (2) : 155-166．
[10] 李才,翟庆国,董永胜,等.青藏高原羌塘中部榴辉岩的发现及其意义[J].科学通报,2006,51(1) :70-74． Li C, Zhai Q G, Dong Y S, et al. The discovery of t he eclogite in Qiangtang area, Tibet [J]. Chinese Science Bulletin, 2006 ,51(1) :70274．
[11] 李才,翟庆国,陈文,等.青藏高原龙木错-双湖板块缝合带闭合的年代学证据--来自果干加年山蛇绿岩与流纹岩Ar-Ar和SHRIMP年龄制约[J].岩石学报,2007,23(5) :911-918． Li C, Zhai Q G,Chen W, et al. Geochronology evidence of the closure of Longmu CoShuanghu suture, Qinghai-Tibet plateau: Ar-Ar and zircon SHRIMP geochronology from ophiolite and rhyolite in Guoganjianian[J]. Acta Petroligca Sinica, 2007,23(5) :911-918．
[12] Hening A. EurPetrographic and Geologie Von Sudwest Tibet [M]. In: Hedin S et. Southern Tibet 5． Stockholm, 1915．
[13] 李才,程立人,胡克,等.西藏龙木错-双湖古特提斯缝合带研究[M].北京:地质出版社,1995． Li C, Cheng L R, Hu K, et al. Study on the paleo-Tethys suture zone of Lungmu Co-Shuanghu, Tibet[M]. Beijing: Geological Publishing House, 1995．
[14] 李才,王天武,杨德明,杨日红.西藏羌塘中央隆起区物质组成与构造演化[J].长春科技大学学报,2001,31(1) :25-31． Li C, Wang T W, Yang D M, et al. The lithological composition and tectonic evolution of Qiangtang central uplift region, Tibet [J]. Journal of Changchun University of Science and Technology, 2001,31(1) :25-31．
[15] 胡克,李才,程立人,等.西藏冈玛错-双湖蓝片岩带及其构造意义[J].长春地质学院学报,1995,23(3) :268-274． Hu K, LI C, Cheng L R, et al. Gangmacuo-Shuanghu blueschist belt in central Qiangtang area of Tibet and it s geological significance[J]. Journal of Changchun University of Earth Sciences, 1995, 23(3) :268-274．
[16] 邓万明,尹集祥,呙中平.羌塘茶布-双湖地区基性超基性岩、火山岩研究[J].中国科学:D辑,1996,26(4) :296-301． Deng W M, Yin J X, Wo Z P. Study on basic-ultrabasic and volcanic rocks of Chabu Shuanghu in Qiangtang[J]. Science in China :Series D,1996,26(4) :2962301．
[17] 鲍佩声,肖序常,王军,等.西藏中北部双湖地区蓝片岩带及其构造涵义[J].地质学报,1999,73(4) :302-314Bao P S, Xiao X C, Wang J, et al. Blueschist belt of Shuanghu area in cent ralnort hern Xizang (Tibet) and it s tectonic implications [J]. Acta Geologica Sinica, 1999, 73 (4) :302-314．
[18] 邓希光,丁林,刘小汉,等.藏北羌塘中部冈玛日-桃形错蓝片岩的发现[J].地质科学,2000,35(2) :227-232． Deng X G, Ding L, Liu X H, et al. Discovery of blueschist s in Gangmar-Taoxing Co area, cent ral Qiangtang, northern Tibet [J]. Scientia Geologica Sinica, 2000, 35 (2) : 227-232．
[19] 邓希光,丁林,刘小汉,等.青藏高原羌塘中部蓝片岩的地球化学特征及其构造意义[J].岩石学报,2002,18(4) :517-525． Deng X G, Ding L, Liu X H, et al. Geochemical characteristics of t he blueshist s and it s tectonic significance in cent ral Qiangtang area , Tibet [J]. Acta PetrologicaSinica,2002,18(4) :517-525．
[20] 李春昱.试谈板块构造[J].西北地质科技情报,1973,第一期(增刊):1-26． Li C Y. Discourse of Plate tectonics [J]. Northwestern Geological Information, 1973,1(Supp.):1-26．
[21] Dobretsov N L. Blueshists and eclogites: a possible plate tectonic mechanism for their emplacement from the upper mantle. Tectonophysics[J]. 1991,186:253-268．
[22] 任纪舜 主编.中国及邻区大地构造图[M].北京:中国地质出版社,1997． Ren J S. The tectonic map of t he Peopleps Republic of China and adjacent area [M]. Beijing: Geological Publishing House, 1997．
[23] 常承法,潘裕生,郑锡澜.青藏高原地质构造,北京:科学出版社,1982． Chang C F, Pan Y S, Zheng X L, et al. The geological tectonics of Qinghai-Xizang (Tibet) plateau. Beijing: Science Press, 1982．
[24] 尹安.喜马拉雅-青藏高原造山带地质演化-显生宙亚洲大陆生长.地球学报,2001,22(3) :193-230． Yin A. Geologic evolution of the Himalayan-Tibtan orogen-Phanerozoic growth of Aisa continetal. Acta Geoscientia Sinica (in Chinese) , 2001, 22(3) : 193-230．
[25] 郭新峰,张元丑,程庆云,等.青藏高原亚东-格尔木地学断面岩石圈电性研究[J].中国地质科学院院报,1990,21:191-202． Guo X F, Zhang Y C, Cheng Q Y, et al. Magnetotelluric studies along Yadong-Golmud geosciences transect in Qinghai-Xizang plateau[J]. Bulletin of The Chinese Academy of Geological Sciences (in Chinese), 1990, 21:191-202．
[26] 秦国卿,陈九辉,刘大建等.昆仑山脉河喀喇昆仑山脉地区的地壳上地幔电性结构特征[J].地球物理学报,1994,37(2) :193-199． Qin G Q, Chen J H, LIU D J, et al. The characteristics of the electrical structure of the crust and upper mantle in the the region of the Kunlun and the Karakorum Mountains[J]. Acta Geophysica Sinica,1994,37(2) : 193-199．
[27] 孔祥儒,王谦身,熊绍柏.青藏高原西部综合地球物理与岩石圈结构的研究[J].中国科学(D辑),1996,26(4) :308-315． Kong X R, Wang Q S, Xiong S B. Comprehensive geophysics and lithospheric st ructure in t he western Xizang (Tibet) plateau [J]. Scince in China:Series D, 1996 , 26 (4) :308-315．
[28] 张胜业,魏胜,王家映,等.西藏羌塘盆地大地电磁测深研究[J].地球科学,1996,21(1) :198-202． Zhang S Y, Wei S, Wang J Y, et al . Magnetotelluric sounding in the Qiangtang basin of Xizang (Tibet) [J]. Earth Science, 1996,21(2) : 1982202．
[29] 鲁兵,徐可强,刘池阳.藏北羌塘地区的地壳电性结构及其意义[J].地学前缘,2003,10(Sup.):153-159． Lu B, Xu KQ, Liu C Y, Electrical structure of crust in the qiangtang region , northern Tibet and its geological significance[J]. Earth Science Frontiers (China University of geosciences, Beijing), 2003． 10 (Sup.): 153-159．
[30] 魏文博,金胜,叶高峰,等.藏北高原地壳及上地幔导电性结构-超宽频带大地电磁测深研究结果[J].地球物理学报,2006,49(4) :1215-1225． Wei W B, Jin S, Ye G F, et al. Conductivity structure of crust and upper mantle beneath the northern Tibetan Plateau: Results of super-wideband magnetotelluric sounding [J]. Chinese J. Geophys. 2006,49(4) : 1215-1225．
[31] Zhao W, Mechie J, Brown, L D, et al. Crustal structure of the central Tibet as derived from project INDEPTH wideangle seismic data [J]. Geophys. J. Int. 2001,145:486-498．
[32] Haines S, Klemperer S L, Brown L, et al. Crustal thickening processes in central Tibet: implications of INDEPTH Ⅲ seismic data[J]. Tectonics 2003, 22:1-18．
[33] Ross A R, Brown L D, Pananont P. et al. Deep reflection surveying in central Tibet: lower-crustal layering and crustal flow[J]. Geophys. J. Int. , 2004, 156:115-128．
[34] 卢占武.青藏高原羌塘盆地岩石圈结构及其对油气远景的影响[博士论文].北京:中国地质科学院,2006． Lu Z W, Lithosphere structure of the Qiangtang basin, Qinghai-Tibetan plateau and its influence on petroleum prospcet[D]. Beijing: Chinese Academy Geological Sciences, 2006．
[35] 卢占武.青藏高原羌塘地体地壳精细结构横剖面-贯穿南北的地震反射探测试验研究[博士后出站报告].中国地质科学院,2008． 12． Lu Z W. The crustal fine structure of the Qiangtang terrance in the Tibetan plateau-Study on the N-S trending seismic reflection profile [Post Ph. D. thesis]. Beijing: Chinese Academy Geological Sciences, 2008． 12．
[36] Wittlinger G, Vergne J, Tapponnier P, et al. Teleseismic imaging of subducting lithosphere and Moho offsets beneath western Tibet. Earth and Planetary Sci. Lett., 2004,221: 117-130．
[37] Wittlinger G, Masson F, Poupinet G, et al. Seismic tomography of northern Tibet and Kunlun: Evidence for crustal blocks and mantle velocity contrasts[J]. Earth and Planetary Science letters, 1996, 139:263-279．
[38] Tilmann F, Ni J. INDEPTH Ⅲ Seismic Team, Seismic imaging of the downwelling Indianlithosphere beneath central Tibet[J]. Science, 2003,300:1424-1427．
[39] He R, Zhao D, Zheng H, et al. Teleseismic P-wave tomography under the central Tibet Plateau (Abstract) , EOS,AGU-2006WPGM, 2006,T12B-04．
[40] Zhao D, Hasegawa A, Horiuchi S. Tomographic imaging of P and S wave velocity structure beneath northeastern Japan [J]. J. Geophys. Res. 1992,97:19909-19928．
[41] Zhao D, Hasegawa A, Kanamori H. Deep structure of Japan subduction zone as derived from local, regional and teleseismic events[J]. J. Geophys. Res. 1994 , 99: 22313-22329．
[42] Zhao D. New advances of seismic tomography and its applications to subduction zones and earthquake fault zones: a review[J]. The Island Ar, 2001c 10, 68-84．
[43] 贺日政,赵大鹏,高锐,等.西昆仑造山带下岩石圈地幔速度结构[J].地球物理学报,2006,49(3) :778-787． He R Z, Zhao D P, Gao R, et al. Teleseismic P-wave tomography of lithospheric mantle beneath west Kunlun orogenic belts[J]. Chinese J. Geophys. (in Chinese), 2006, 49(3) :778-787．
[44] 郑洪伟.青藏高原地壳上地幔三维速度结构及其地球动力学意义[博士论文].北京:中国地质科学院,2006． Zheng H W. 3-D velocity structure of the crust and upper mantle in Tibet and its geodynamic effect [Ph. D. thesis]. Beijing:Chinese Academy Geological Sciences,2006．
[45] 郑洪伟,李廷栋,高锐,等.印度板块岩石圈地幔向北俯冲到羌塘地体之下的远震P波层析成像证据[J].地球物理学报,2007,50(5) :1418-1426． Zheng H W, Li T D, Gao R, et al. , Teleseismic P-wave tomography evidence for the Indian lithospheric mantle subducting northward beneath the Qiangtang terrane [J]. Chinese Journal of Geophysics,2007 ,50(5) : 1418-1426．
[46] Tian X B, Wu Q J, Zhang Z J, et al. Joint imaging by teleseismic converted and multiple waves and its applicaton in the IND EPTH-Ⅲ passive seismic arry [J]. Geophysical Research Letters, 2005, 32(L21315) , doi: 10． 1029/2005GL023686．
[47] Willett S D, Beaumont C. Subduction of Asian lithospheric mantle beneath Tibet inferred from models of continental collision[J]. Nature, 1994,369:642-645．
[48] 滕吉文,张中杰,万志超,等.羌塘盆地及周边地带地球物理场与油气深部构造背景初探[J].地球物理学进展,1996,11(1) :12-27． Teng J W, Zhang Z J, Wan Z C, et al. The preliminary study of geophysical field and deep structural background of oil and gas for Qiangtang Basin and its neighboring regions [J]. Geophysical Development ,1996 ,11(1) :15216．
[49] 贺日政.青藏高原近南北向裂谷的岩石圈结构及其动力学过程[博士论文].北京:中国地质科学院,2003． He R Z. Lithospheric Structure of near north-south striking rifts in tibet plateau and its geodynamical process [Ph. D. thesis]. Beijing: Chinese Academy Geological Sciences, 2003．
[50] 刘池阳,杨兴科,魏永佩,等.藏北羌塘盆地西部查桑地区结构及结构特征[J].地质论评,2002,48(6) :593-602． Liu C Y, Yang X K, Wei Y P, et al. Structure and tectonic feature of Chasang area in west part of Qiangtang basin, north part of Tibet[J]. Geologcial review, 2002 ,48(6) :593-602．
[51] 王喜臣,贾建秀,徐宝慈.羌塘拗陷石油地质走廊剖面重磁异常处理模拟及地质解释[J].吉林大学学报(地球科学版),2008,38(4) :685-691． Wang X C, Jia J X, XU B C. Gravity/Magnetic modeling and geological explanation in Qiangtang Basin geologic aisle [J]. Journal of Jilin University (Earth Science Edition), 2008, 38 (4) :685-691．
[52] 苑守成,于国明,田黔宁.青藏高原羌塘盆地重磁剖面异常与基底构造特征[J].地质通报,2007,26(6) :703-709． Yuan S C, Yu G M, Tian Q N. Gravity and magnetic anomaly profiles and characteristics of basement structure in the Qiangtang basin[J]. Qinghai-Tibet Plateau, Geological Bulletin of China, 2007, 26(6) :703-709．
[53] 田黔宁,耿涛,杨汇群,等.青藏高原西部重力异常剖面拟合及其地质解释[J].地质通报,2008,27(12) :2108-2116． Tian Q N, Geng T, Yang H Q, et al. Gravity anomalies forward fitting and geological explanation in the western Qinghai-Tibet Plateau [J]. Geologcial Bulletin of China, 2008,27(12) :2108-2116．
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