ESR DATING OF THE PALAEOGENE IN MULI BASIN IN THE MIDDLE OF QILIAN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE

QI Bang-shen; HU Dao-gong; WANG Jin-shou; ZHAO Xi-tao; ZHANG Xu-jiao; ZHANG Yao-ling; YANG Xiao-xiao; GAO Xue-mi

Volume 19 Issue 4

Dec. 2013

Turn off MathJax

Article Contents

Abstract

References

Article Navigation > Journal of Geomechanics > 2013 > 19(4): 392-402

QI Bang-shen, HU Dao-gong, WANG Jin-shou, et al., 2013. ESR DATING OF THE PALAEOGENE IN MULI BASIN IN THE MIDDLE OF QILIAN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE. Journal of Geomechanics, 19 (4): 392-402.

Citation:

PDF( 2334 KB)

ESR DATING OF THE PALAEOGENE IN MULI BASIN IN THE MIDDLE OF QILIAN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE

1.
School of Earth Science and Resources, China University of Geosciences, Beijing 100029, China
2.
Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China
3.
Qinghai Institute of Geological Survey, Xining 810017, China
4.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

More Information

Abstract

Abstract

The technique of ESR was applied to determine the Cenozoic red beds, Muli Basin, therefore, we can get the age of sedimentary and tectonic deformation. The results indicated there were huge thick Cenozoic Red Beds and tectonic deformation geochronological data, well recording the uplift of Qilian Mountains. Based on the ESR dating, the Tertiary sediments include the Eocene to Oligocene Huoshaogou Formation (40.2~35.3 Ma), which consists mainly of lacustrine facies and the Oligocene Baiyanghe Formation (32.6~24.3 Ma), which consists lacustrine and fluvial facies. From late Eocene to early Oligocene, an obvious angular unconformity exists between the upper and lower strata and it can be inferred that Qilian Mountains area has been a tectonic deformation and uplift, which has corresponding connection with the early Cenozoic uplift of Qilian Mountains.
- Baiyanghe Formation,
- Huoshaogou Formation,
- ESR dating,
- the middle of Qilian Mountains

FullText(HTML)

References(44)

References

[1]	潘保田, 李吉均, 陈发虎.青藏高原:全球气候变化的驱动机和放大器-Ⅰ:新生代气候变化的基本特征[J].兰州大学学报:自然科学版, 1995, 31(3):120~128. PAN Bao-tian, LI Ji-jun, CHEN Fa-hu. Qinghai-Tibetan Plateau:A driver and amplifier of global climatic changes-Ⅰ:Basic characteristics of climatic changes in Cenozoic Era[J]. Journal of Lanzhou University:Natural Sciences, 1995, 31(3):120~128.
[2]	潘保田, 李吉均, 朱俊杰, 等.青藏高原:全球气候变化的驱动机和放大器-Ⅱ:青藏高原隆升的基本过程[J].兰州大学学报:自然科学版, 1995, 31(4):160~167. http://cdmd.cnki.com.cn/Article/CDMD-10730-2008162364.htm PAN Bao-tian, LI Ji-jun, ZHU Jun-jie, et al. Qinghai-Tibetan Plateau:A driver and amplifier of global climatic changes-Ⅱ:Uplift processes of the Qinghai-Xizang (Tibetan) Plateau[J]. Journal of Lanzhou University:Natural Sciences, 1995, 31(4):160~167. http://cdmd.cnki.com.cn/Article/CDMD-10730-2008162364.htm
[3]	潘保田, 李吉均.青藏高原:全球气候变化的驱动机和放大器-Ⅲ:青藏高原隆起对气候变化的影响[J].兰州大学学报:自然科学版, 1996, 32(1):108~115. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK601.023.htm PAN Bao-tian, LI Ji-jun. Qinghai-Tibetan Plateau:A driver and amplifier of global climatic changes-Ⅲ:The effects of the uplift of Qinghai-Tibetan Plateau on climatic changes[J]. Journal of Lanzhou University:Natural Sciences, 1996, 32(1):108~115. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK601.023.htm
[4]	李东旭.大陆边缘反S状造山带三维模式兼论青藏高原结构与隆升[J].地质力学学报, 2007, 13(1):31~41. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070105&journal_id=dzlxxb LI Dong-xu. 3D model of reversed S-shaped orogenic belts on the continental margin:With a discussion of the internal structure and uplift of the Qinghai-Tibet Plateau[J]. Journal of Geomechanics, 2007, 13(1):31~41. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070105&journal_id=dzlxxb
[5]	朱大岗, 孟宪刚, 赵希涛, 等.西藏纳木错盆地116ka以来沉积演化与青藏高原隆升[J].地质力学学报, 2005, 11(2):172~180. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20050226&journal_id=dzlxxb ZHU Da-gang, MENG Xian-gang, ZHAO Xi-tao, et al. Sedimentary evolution of the Namco Basin, Tibet, since 116ka BP and Qinghai-Tibet Plateau uplift[J]. Journal of Geomechanics, 2005, 11(2):172~180. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20050226&journal_id=dzlxxb
[6]	李吉均, 文世宣, 张青松, 等.青藏高原隆升的时代、幅度和形式的探讨[J].中国科学, 1979, (6):608~616. http://www.cnki.com.cn/Article/CJFDTOTAL-JAXK197906008.htm LI Ji-jun, WEN Shi-xuan, ZHANG Qing-song, et al. The age, range and forms of the Qinghai-Tibet plateau uplift[J]. Science in China, 1979, (6):608~616. http://www.cnki.com.cn/Article/CJFDTOTAL-JAXK197906008.htm
[7]	李吉均, 方小敏.青藏高原隆升与环境变化研究[J].科学通报, 1998, 43(15):1569~1574. doi: 10.3321/j.issn:0023-074X.1998.15.001 LI Ji-jun, FANG Xiao-min. The Qinghai-Tibet plateau uplift and environmental change research[J]. Chinese Science Bulletin, 1998, 43(15):1569~1574. doi: 10.3321/j.issn:0023-074X.1998.15.001
[8]	丁林, 钟大赉, 潘裕生, 等.东喜马拉雅构造结上新世以来快速抬升的裂变径迹证据[J].科学通报, 1995, 40(16):1479~1500. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199516017.htm DING Lin, ZHONG Da-lai, PAN Yu-sheng, et al. The fission track evidence about eastern Himalayan tectonic rapid uplift since Pliocene[J]. Chinese Science Bulletin, 1995, 40(16):1479~1500. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199516017.htm
[9]	钟大赉, 丁林.青藏高原的隆升过程及其机制探讨[J].中国科学:D辑, 1996, 26(4):289~295. ZHONG Da-lai, DING Lin. The Qinghai-Tibet plateau uplift process and its mechanism[J]. Science in China:Edition D, 1996, 26(4):289~295.
[10]	Harrison T M, Copeland P, Kidd W S F, et al. Activation of the Nyainqentanghla shear zone:Implications for uplift of the southern Tibetan Plateau[J]. Tectonics, 1995, 14(3):658~676. doi: 10.1029/95TC00608
[11]	Blisniuk M P, Hacker R B, Glodny J, et al. Normal faulting in central Tibet since at least 13.5 Ma ago[J]. Nature, 2001, 412:628~632.
[12]	Coleman M, Hodges K. Evidence for Tibetan Plateau uplifted before 14 Myr ago from a new minimal age for east-west extension[J]. Nature, 1995, 374:49~52. doi: 10.1038/374049a0
[13]	Turner S, Arnaud N, Liu L, et al. Post-collision, shoshonitic volcanism on the Tibetan Plateau:Implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Journal of Petrology, 1996, 37:45~71. doi: 10.1093/petrology/37.1.45
[14]	Rowley D B, Currie B S. Paleo-altimetry of the late Eocene to Miocene Lunpola Basin, central Tibet[J]. Nature, 2006, 439:677~681. doi: 10.1038/nature04506
[15]	吴珍汉, 吴中海, 胡道功, 等.青藏高原渐新世晚期隆升的地质证据[J].地质学报, 2007, 81(5):577~587. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200705000.htm WU Zhen-han, WU Zhong-hai, HU Dao-gong, et al. Geological evidences for the Tibetan Plateau uplifted in late Oligocene[J]. Acta Geologica Sinica, 2007, 81(5):577~587. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200705000.htm
[16]	Tapponnier P, Xu Z Q, Francoise R, et al. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science, 2001, 294:1671~1677. doi: 10.1126/science.105978
[17]	Meyer B, Tapponnier P, Bourjot L, et al. Crustal thickening in Gansu-Qinghai, lithospheric mantle subduction, and oblique, strike-slip controlled growth of the Tibet plateau[J]. Geophysical Journal International, 1998, 135(1):1~47. doi: 10.1046/j.1365-246X.1998.00567.x
[18]	Yin A, Harrison T M. Geologic evolution of the Himalayan-Tibetan orogen[J]. Annual Review of Earth Planet Science, 2000, 28:211~280. doi: 10.1146/annurev.earth.28.1.211
[19]	Yin A, Rumelhrt P E, Bulter R, et al. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation[J]. GSA Bulletin, 2002, 114(10):1257~1295. doi: 10.1130/0016-7606(2002)114<1257:THOTAT>2.0.CO;2
[20]	陆洁民, 郭召杰, 赵泽辉, 等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报, 2004, 10(1):50~61. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200401003.htm LU Jie-min, GUO Zhao-jie, ZHAO Ze-hui, et al. Cenozoic sedimentary characteristics of Jiuxi Basin and its relationship with uplift of Qilian Mountains[J]. Geological Journal of China Universities, 2004, 10(1):50~61. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200401003.htm
[21]	戴霜, 方小敏, 宋春晖, 等.青藏高原北部的早期隆升[J].科学通报, 2005, 50(7):673~683. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200507011.htm DAI Shuang, FANG Xiao-min, SONG Chun-hui, et al. Northern Qinghai-Tibet Plateau early uplift[J]. Chinese Science Bulletin, 2005, 50(7):673~683. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200507011.htm
[22]	Wang E Q. Displacement and timing along the northern strand of the Altyn Tagh fault zone, northern Tibet[J]. Earth and Planetary Science Letters, 1997, 150(1-2):55~64. doi: 10.1016/S0012-821X(97)00085-X
[23]	郑德文, 张培震, 万景林, 等.六盘山盆地热历史的裂变径迹证据[J].地球物理学报, 2005, 48(1):157~164. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200501021.htm ZHENG De-wen, ZHANG Pei-zhen, WAN Jing-lin, et al. Apatite fission track evidence for the thermal history of the Liupanshan Basin[J]. Chinese Journal of Geophysics, 2005, 48(1):157~164. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200501021.htm
[24]	张培震, 郑德文, 尹功明, 等.有关青藏高原东北缘晚新生代扩展与隆升的讨论[J].第四纪研究, 2006, 26(1):5~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601001.htm ZHANG Pei-zhen, ZHENG De-wen, YIN Gong-ming, et al. Discussion on late Cenozoic growth and rise of northeastern margin of the Tibetan Plateau[J]. Quaternary Sciences, 2006, 26(1):5~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601001.htm
[25]	Meng Q R, Hu J M, Yang F Z. Timing and magnitude of displacement on the Altyn Tagh fault:Constraints from stratigraphic correlation of adjoining Tarim and Qaidam basins, NW China[J]. Terra Nova, 2001, 13(2):86~91. doi: 10.1046/j.1365-3121.2001.00320.x
[26]	Gilder S, Chen Y, Sen S. Oligo-Miocene magnetostratigraphy and rock magnetism of the Xishuigou section, Subei (Gansu Province, western China) and implications on shallow inclinations in central Asia[J]. Journal of Geophysical Reasearch:Solid Earth, 2001, 106:30505~30521. doi: 10.1029/2001JB000325
[27]	Wang X M, Wang B Y, Qiu Z X, et al. Danghe area (western Gansu, China) biostratigraphy and implications for depositional history and tectonics of northern Tibetan Plateau[J]. Earth and Planetary Science Letters, 2003, 208(3/4):253~269.
[28]	张雪亭, 杨生德, 杨站君, 等.青海省区域地质概论[M].北京:地质出版社, 2007:72~82. ZHANG Xue-ting, YANG Sheng-de, YANG Zhan-jun, et al. The regional geology of Qinghai Province[M]. Beijing:Geological Publishing House, 2007:72~82.
[29]	孙红波, 孙军飞, 张发德, 等.青海木里煤田构造格局与煤盆地构造演化[J].中国煤炭地质, 2009, 21(12):34~37. doi: 10.3969/j.issn.1674-1803.2009.12.010 SUN Hong-bo, SUN Jun-fei, ZHANG Fa-de, et al. Structural framework and coal basin tectonic evolution in Muli Coalfield, Qinghai[J]. Coal Geology of China, 2009, 21(12):34~37. doi: 10.3969/j.issn.1674-1803.2009.12.010
[30]	张克信, 王国灿, 季军良, 等.青藏高原古近纪-新近纪地层分区与序列及其对隆升的响应[J].中国科学:地球科学, 2010, 40(12):1632~1654. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201012003.htm ZHANG Ke-xin, WANG Guo-can, JI Jun-liang, et al. Paleogene-Neogene stratigraphic realm and sedimentary sequence of the Qinghai-Tibet Plateau and their response to uplift of the plateau[J]. Science China:Earth Sciences, 2010, 53:1271~1294. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201012003.htm
[31]	宋春晖. 青藏高原北缘新生代沉积演化与高原构造隆升过程[D]. 兰州: 兰州大学, 2006: 1~326. http://d.wanfangdata.com.cn/Thesis/Y1009009 SONG Chun-hui. Teetonic uplift and Cenozoic sedimentary evolution in the northern margin of the Tibetan Plateau[D]. Lanzhou:Lanzhou University, 2006:1~326. http://d.wanfangdata.com.cn/Thesis/Y1009009
[32]	岳乐平, Heller E, 邱占祥, 等.兰州盆地第三系磁性地层年代与古环境记录[J].科学通报, 2000, 45(18):1998~2003. doi: 10.3321/j.issn:0023-074X.2000.18.019 YUE Le-ping, Heller E, QIU Zhan-xiang, et al. Lanzhou basin, Tertiary magnetic formations and paleoenvironment records[J]. Chinese Science Bulletin, 2000, 45(18):1998~2003. doi: 10.3321/j.issn:0023-074X.2000.18.019
[33]	Williams M A J, Dunkerley D L, Deckker P D, 等.第四纪环境[M].刘东升, 编译.北京:科学出版社, 1997:190. Williams M A J, Dunkerley D L, Deckker P D, et al. Quaternary environment[M]. LIU Dong-sheng, ed. Beijing:Science Press, 1997:190.
[34]	程强, 寇小兵, 黄绍槟, 等.中国红层的分布及地质环境特征[J].工程地质学报, 2004, 12(1):34~40. http://www.cnki.com.cn/Article/CJFDTOTAL-GCDZ200401006.htm CHENG Qiang, KOU Xiao-bing, HUANG Shao-bin, et al. The distributes and geologic environment characteristics of red beds in China[J]. Journal of Engineering Geology, 2004, 12(1):34~40. http://www.cnki.com.cn/Article/CJFDTOTAL-GCDZ200401006.htm
[35]	Lee T Y, Lawver L A. Cenozoic plate reconstruction of Southeast Asia[J]. Tectonophysics, 1995, 251(1-4):85~138. doi: 10.1016/0040-1951(95)00023-2
[36]	Patzelt A, Li H M, Wang J D, et al. Palaeomagnetism of Cretaceous to Tertiary sediments from southern Tibet:Evidence for the extent of the northern margin of India prior to the collision with Eurasia[J]. Tectonophysics, 1996, 259(4):259~284. doi: 10.1016/0040-1951(95)00181-6
[37]	Beck R A, Burbank D W, Sercombe W J, et al. Stratigraphic evidence for an early collision between northwest India and Asia[J]. Nature, 1995, 373:55~58. doi: 10.1038/373055a0
[38]	Dewey J F, Shackleton R M, Chang C F, et al. The tectonic evolution of the Tibetan Plateau[J]. Philosophical Transactions of Royal Society A:Mathematical, Physical and Engineering Sciences, 1988, 327(1594):379~413. doi: 10.1098/rsta.1988.0135
[39]	Liu Z, Wang C S, Yi H S. Evolution and mass accumulation of the Cenozoic Hoh Xil Basin, northern Tibet[J]. Journal of Sedimentary Research, 2001, 71(6):971~984. doi: 10.1306/030901710971
[40]	刘志飞, 王成善, 伊海生, 等.可可西里盆地新生代沉积演化历史重建[J].地质学报, 2001, 75(2):250~258. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200102017.htm LIU Zhi-fei, WANG Cheng-shan, YI Hai-sheng, et al. Reconstruction of depositional history of the Cenozoic Hoh Xil Basin[J]. Acta Geologica Sinica, 2001, 75(2):250~258. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200102017.htm
[41]	刘志飞, 王成善, 伊海生, 等. 青藏高原北部可可西里盆地早新生代沉降史及其高原隆升意义[C]//陈毓川. 中国地质学会80周年学术文集. 北京: 地质出版社, 2002: 111~119. LIU Zhi-fei, WANG Cheng-shan, YI Hai-sheng, et al. Early Cenozoic subsidence history of the Hoh Xil Basin in the northern Qinghai-Tibetan Plateau[C]//CHEN Yu-chuan. Academic papers of the 80^th anniversary of the Geological Society of China. Beijing:Geological Publishing House, 2002:111~119.
[42]	刘志飞, 王成善.青藏高原北部可可西里盆地第三纪风火山群沉积环境分析[J].沉积学报, 2001, 19(1):28~36. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200101004.htm LIU Zhi-fei, WANG Cheng-shan. Depositional environment of the Tertiary Fenghuoshan Group in the Hoh Xil Basin, northern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2001, 19(1):28~36. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200101004.htm
[43]	刘志飞, Stewart L K.图形显示和比较古水流数据的一种软件(PC99):以青藏高原北部可可西里盆地新生代古水流数据为例[J].沉积学报, 2002, 20(2):354~358. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200202027.htm LIU Zhi-fei, Stewart L K. A software tool for graphically displaying and comparing palaeocurrent data (PC99):An example utilizing palaeocurrent data of the Cenozoic Hoh Xil Basin, northern Tibet[J]. Acta Sedimentologica Sinica, 2002, 20(2):354~358. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200202027.htm
[44]	刘志飞, 王成善, 金玮, 等.青藏高原沱沱河盆地渐新世-中新世沉积环境分析[J].沉积学报, 2005, 23(2):210~217. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200502004.htm LIU Zhi-fei, WANG Cheng-shan, JIN Wei, et al. Oligo-Miocene depositional environment of the Tuotuohe Basin, Central Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2005, 23(2):210~217. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200502004.htm

Relative Articles

	ZHANG Xiaoyin, ZHAN Rongruo, DUAN Liang, LUO Xiaorong, WEI Ronghao. 2024: 3D digital modelling and detailed anatomy of tight sandstone reservoir outcrop with oil-bearing heterogeneity: A case study of Angou outcrop of Triassic Yanchang Formation in Ordos Basin. Journal of Geomechanics, 30(4): 609-621. doi: 10.12090/j.issn.1006-6616.2024028
	WANG Guanmin, ZHU Xinyi, LIU Hai, CHEN Shuai, SHI Xiaoming, HU Jin. 2024: The application of sedimentary microfacies on the fracability of tight sandstone reservoir in Chang 7 member of Longdong area in the Ordos Basin. Journal of Geomechanics, 30(6): 893-905. doi: 10.12090/j.issn.1006-6616.2024004
	LIU Zhihui, LIU Xiaochun, CHEN Longyao, ZHENG Guanggao, HU Juan. 2024: Zircon U-Pb dating of the Dizhuanggou Formation, Changjiaoba Group in the South Qinling Belt and its tectonic significance. Journal of Geomechanics, 30(6): 1012-1027. doi: 10.12090/j.issn.1006-6616.2024027
	LIU Jin, WANG Jian, TAN Jingqiang, CUI Haisu, LIU Miao, ZHENG Yu, SONG Xueqi, YUAN Qiang. 2023: Sedimentary paleo-environment and organic matter enrichment in the Lucaogou Formation of the Jimsar Sag. Journal of Geomechanics, 29(5): 631-647. doi: 10.12090/j.issn.1006-6616.2022127
	LI Bo, SONG Yixin, GAO Han, WU Xuan, GUAN Qin, LIU Chunwei. 2021: Hydrogeological characteristics and water yield pattern of the Paleogene Zhujiagou formation in south-central Shandong Province. Journal of Geomechanics, 27(1): 117-126. doi: 10.12090/j.issn.1006-6616.2021.27.01.012
	YU Xin, LI Gao, CHEN Ze, ZHANG Yi. 2021: Experimental study on physical and mechanical characteristics of tight sandstones in the Xujiahe Formation in western Sichuan after high-temperature exposure. Journal of Geomechanics, 27(1): 1-9. doi: 10.12090/j.issn.1006-6616.2021.27.01.001
	XIA Mengmeng, WANG Chaoqun, HU Daogong, ZHAO Xitao, JIA Liyun, WU Huanhuan, LYU Tongyan. 2019: ESR DATING OF THE BASUO FORMATION IN THE NORTHEASTERN HAINAN ISLAND AND ITS TECTONIC SIGNIFICANCE. Journal of Geomechanics, 25(2): 257-266. doi: 10.12090/j.issn.1006-6616.2019.25.02.025
	ZHANG Yaoling, SHEN Yanxu, WU Zhenhan, ZHAO Zhen. 2018: ZIRCON U-PB AGES OF MAGMATIC ROCKS FROM MEISU FORMATION IN GERZE AREA IN TIBET AND ITS GEOLOGICAL SIGNIFICANCE. Journal of Geomechanics, 24(1): 128-136. doi: 10.12090/j.issn.1006-6616.2018.24.01.014
	XIONG Jin-hong, CHEN Cen, CAO Zhan-yuan, TAN Xian-feng, KUANG Hao. 2017: FRACTURE DEVELOPMENT PREDICTION BASED ON AZIMUTHAL ANISOTROPY ANALYSIS OF PRE-STACK SEISMIC-TAKE XUJIAHE FORMATION OF PUGUANG GAS FIELD FOR EXAMPLE. Journal of Geomechanics, 23(2): 280-287.
	LI Bing, ZHANG Yao-ling, WANG Chao-qun, HU Dao-gong. 2016: GEOCHEMICAL CHARACTERISTICS OF THE YOUHULUGOU BASALTS IN THE SUTURE ZONE OF THE NORTH QILIAN MOUNTAIN. Journal of Geomechanics, 22(1): 48-55.
	MIAO Feng-bin, ZENG Lian-bo, ZU Ke-wei, GONG Lei. 2016: CHARACTERISTICS AND CONTROLLING FACTORS OF FRACTURES IN RESERVOIRS OF XUJIAHE FORMATION IN ZITONG AREA, SICHUAN BASIN. Journal of Geomechanics, 22(1): 76-84.
	XU Jiu-sheng, WEN Zhi-gang, HU Dao-gong, ZHANG Yao-ling, QI Bang-shen. 2015: EVALUATION OF THE HYDROCARBON GENERATION POTENTIAL OF SOURCE ROCKS OF THE JURASSIC YAOJIE FORMATION IN MULI DEPRESSION OF QILIAN MOUNTAINS. Journal of Geomechanics, 21(3): 446-452.
	ZHAO Li-guo, YANG Xiao-ping, ZHAO Xing-min, LIU Yuan, ZHANG Wei-long. 2014: LA-ICP-MS U-Pb GEOCHRONOLOGY OF THE SEDIMENTARY ROCK AND VOLCANO ROCK ZIRCONS FROM THE EMOERHE GROUP IN THE MOHE BASIN AND ITS GEOLOGICAL SIGNIFICANCE. Journal of Geomechanics, 20(3): 285-291.
	LIAO Hua, HU Dao-gong, ZHANG Xu-jiao, YU Wen-lin, GUO Tao. 2014: ZIRCON U-Pb AGE FOR GRANITE OF THE ORDOVICIAN FORMATION AND ITS TECTONIC SIGNIFICANCE IN THE SOUTHERN QILIAN. Journal of Geomechanics, 20(3): 292-298.
	LIU Xiao-jia, ZHAO Li-guo, TIAN Jun, YANG Xiao-ping, ZHANG Wen-long, GAO Xue-mi. 2014: ESR AGES EVIDENCES OF MOHE OVERTHRUST STRUCTURE STAGE. Journal of Geomechanics, 20(3): 299-303.
	YANG Yan, YANG Bo, ZHANG Hong-yuan. 2013: MICROTECTONIC FEATURES AND EVOLUTION OF THE YUSHIGOU PERIDOTITE ROCK FROM THE QILIANSHAN MOUNTAIN. Journal of Geomechanics, 19(3): 275-286.
	JIANG Fu-chu, FU Jian-li, WANG Shu-bing, LI Chao-zhu. 2013: DISCUSSION ON THE EPOCH OF LACUSTRINE STRATA IN TOGTOH, INNER MONGOLIA. Journal of Geomechanics, 19(1): 1-13.
	GUO Wei, YANG Xinde, ZHANG Juan, HAO Bin. 2011: GEOCHEMICAL CHARACTERISTICS OF CLASTIC SEDIMENTARY ROCKS FROM LOWER PERMIAN YUJIABEIGOU FORMATION IN NORTHERN CHIFENG, INNER MONGOLIA. Journal of Geomechanics, 17(3): 295-302.
	WU Fang, ZHANG Xu-jiao, ZHANG Yong-qing, ZHANG Yao-ling. 2010: ZIRCON U-Pb AGES FOR RHYOLITIC TUFFS OF THE NAOCANGJIANGOU FORMATION IN THE EAST KULUN OROGENIC BELT AND THEIR IMPLICATION. Journal of Geomechanics, 16(1): 44-50.
	Zhang Shukun, Sun Jiashu, Wang Xihai, Feng Yanwei. 1996: SER DATING OF THE F1 AND F7 FAULTS IN THE ZHANGHEWAN RESERVOIR DISTRICT, HEBEI. Journal of Geomechanics, 2(2): 94-96.

Supplements(0)

Cited By

Proportional views

Proportional views

Figures(4) / Tables(2)

Get Citation

PDF

XML

Article Metrics

Article views (239) PDF downloads(13)

ESR DATING OF THE PALAEOGENE IN MULI BASIN IN THE MIDDLE OF QILIAN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE

Abstract

References

Relative Articles

Proportional views

Catalog

Article Metrics

Proportional views

Related

ESR DATING OF THE PALAEOGENE IN MULI BASIN IN THE MIDDLE OF QILIAN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE

Abstract

References

Relative Articles

Proportional views

Catalog

Article Metrics

Proportional views

Related

Export File

Citation

Format

Content