2010 Vol. 16, No. 1

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DISCOVERY OF THE EARLY PLEISTOCENE KUNLUNHE CONGLOMERATE IN GOLMUD OF QINGHAI PROVINCE AND ITS GEOLOGICAL SIGNIFICANCE
ZHAO Xi-tao, HU Dao-gong, WU Zhong-hai, LIU Qi-sheng, ZHANG Yao-ling, XUE La-mei
2010, 16(1): 1-10.
Abstract (463) HTML (401) PDF (640KB)(12)
Abstract:
The Kunlun River originating in the Kunlun Mountains is one of main tributaries of the Golmud River. The reported Neocene and Quaternary strata are mainly distributed in the Kunlun Pass area, whereas in the valley of the Kunlun-Golmud River only occur the strata younger than the Middle Pleistocene. ...
TECTONIC ENVIRONMENT OF NAIJ TAL GROUP IN THE EAST KUNLUN OROGENIC BELT
NI Jin-yu, HU Dao-gong, ZHOU Chun-jing
2010, 16(1): 11-20.
Abstract (253) HTML (129) PDF (351KB)(9)
Abstract:
The Naij Tal Group, an important stratigraphic unit, is of great significance to reconstruction of the geological evolution of the East Kunlun orogenic belt during the Early Paleozoic, but divergent opinions have been proposed about its tectonic environment. Based on close geological survey, a geoch...
SHRIMP ZIRCON U-Pb AGES OF RHYOLITE FROM THE NAIJ TAL GROUP IN THE EAST KULUN OROGENIC BELT
ZHANG Yao-ling, ZHANG Xu-jiao, HU Dao-gong, SHI Yu-ruo, LU Lu
2010, 16(1): 21-27, 50.
Abstract (386) HTML (231) PDF (737KB)(11)
Abstract:
The Naij Tal Group is a major lithostratigraphic unit with a complex composition in the East Kunlu Paleozoic orogenic belt, and there has long been debate on its formation time. The An average SHRIMP zircon 206Pb/238U age of 450.4 ± 4.3 Ma has been obtained for 15 rhyolite samples collected from the...
ZIRCON U-Pb DATING OF THE RHYOLITE-DACITE PORPHYRY IN THE SANDAOWAN OF EAST KUNLUN MOUNTAINS AND ITS GEOLOGICAL SIGNIFICANCE
ZHOU Chun-jing, HU Dao-gong, BAROSH P J, WU Zhen-han, ZHANG Yong-qing, GENG Jian-zhen, HAO Shuang, NI Jin-yu, ZHANG Yao-ling
2010, 16(1): 28-35.
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Abstract:
The Sandaowan rhyolite-dacite porphyry, located to the west of the Golmud River, about 55 km from south of Golmud City, is an intrusive vein of volcanic craters. It intruded into the clastic rocks, named Habalayigou group as one of the Nachitai unit in this region. A sample No. B727-1 was collected ...
ZIRCON U-Pb AGE FROM SYNTECTONIC GRANITIC PORPHYRY IN THE MIDDLE KUNLUN FAULT BELT AND ITS TECTONIC SIGNIFICANCE
LU Lu, HU Dao-gong, ZHANG Yong-qing, WU Zhen-han
2010, 16(1): 36-43.
Abstract (216) HTML (158) PDF (657KB)(5)
Abstract:
A measurement by LA-MC-ICP MS for two samples of zircon from granitic porphyry collected at Golmud, in south part of the middle Kunlun fault belt has yielded two U-Pb ages of 408.5 ± 2.3Ma and 391.2 ± 3.4Ma, respectively. The results show that the middle Kunlun fault belt should be a newly generated...
ZIRCON U-Pb AGES FOR RHYOLITIC TUFFS OF THE NAOCANGJIANGOU FORMATION IN THE EAST KULUN OROGENIC BELT AND THEIR IMPLICATION
WU Fang, ZHANG Xu-jiao, ZHANG Yong-qing, ZHANG Yao-ling
2010, 16(1): 44-50.
Abstract (308) HTML (161) PDF (516KB)(9)
Abstract:
By using La-Mc-ICPMC method, accurate zircon U-Pb dating has been made for volcanic rock samples from the Naocangjiangou Formation in the Xiugou basin of the East Kunlun orogenic belt. The zircons from the rhyolitic tuff (sample DG25-4) showed oscillatory girdles in its cathodeluminescence image, in...
EVIDENCE OF ZIRCON U-Pb AGES FOR THE FORMATION TIME OF THE EAST KUNLUN LEFT-LATERAL DUCTILE SHEAR BELT
ZHANG Zi-cheng, ZHANG Xu-jiao, GAO Wan-li, HU Dao-gong, LU Lu
2010, 16(1): 51-58.
Abstract (324) HTML (144) PDF (680KB)(4)
Abstract:
The large-scale East Kunlun left-lateral ductile shear belt was formed by an oblique collision between the Bayan Har-Songpan-Ganzi terrain and the southern East Kunlun terrain during the Late Triassic. During the Cenozoic, this ductile shear belt was transformed into a brittle leftlateral strike-sli...
EXTRACTION OF LITHOLOGIC INFORMATION FROM THE EAST KULUN OROGENIC BELT USING ASTER REMOTE SENSING IMAGE
GAO Wan-li, ZHANG Xu-jiao, WANG Zhi-gang, ZHANG Zhi-cheng, ZHANG Yao-ling
2010, 16(1): 59-69.
Abstract (231) HTML (122) PDF (1142KB)(7)
Abstract:
By using ASTER data and such methods for extraction of lithologic information as major composition image and the mineral index, a discrimination for and extraction of lithologic information has been made in the Wenquan Reservoir area of the East Kunlun orogenic belt. The results show that the major ...
APPLICATION OF REMOTE SENSING TECHNIQUE IN THE MAPPING OF CENOZOIC GEOLOGY OF THE EAST KUNLUN MOUNTAINS
XUE La-mei, ZHAO Xi-tao, ZHANG Yao-ling, GAO Wan-li
2010, 16(1): 70-77.
Abstract (239) HTML (113) PDF (622KB)(5)
Abstract:
According to the color variations of different geological bodies in the same wave band or the same geological body in different wave bands, a close geological interpretation has been made for the ETM images from the East Wenquan Basin of the east Kunlun Mountains, resulting in the establishment of i...
WULING OROGENY IN EASTERN GUIZHOU AND ITS ADJACENT REGIONS AND ITS GEOLOGICAL SIGNIFICANCE
DAI Chuan-gu, CHEN Jian-shu, LU Ding-biao, MA Hui-zhen, WANG Xue-hua
2010, 16(1): 78-84.
Abstract (236) HTML (94) PDF (632KB)(12)
Abstract:
The Wuling orogeny made a significant influence in eastern Guizhou and its adjacent regions, as reflected by the appearance of disconformities between middle and upper Proterozoic. It took its most profound expression in northern section of the Fanjing Mountain of Guizhou Province, Dayong, Yueyang a...
SEDIMENTARY CHARACTERISTICS OF THE JIUFOTANG FORMATION DEVELOPED IN LUANPING MESOZOIC FAULT BASIN OF NORTHERN HEBEI PROVINCE
PAN Li-cheng, LI Lin-qing, LI Xiang, WU Geng-lin, ZHAO Hai-xuan
2010, 16(1): 85-95.
Abstract (266) HTML (181) PDF (811KB)(8)
Abstract:
In the Luanping area of northern Hebei Province, there appears a Mesozoic continental fault basin. Its uppermost part is occupied by the Early Cretaceous Jiufotang Formation, which consists of tremendously thick grayish green-grayish yellow clastic rocks formed under inland warmhumid climate. In gen...
GEOCHEMISTRY AND GENESIS OF BASIC-INTERMEDIATE VOLCANIC ROCKS FROM KALADAWAN, EAST ALTUN TAGH MOUNTAINS
CUI Ling-ling, CHEN Bai-lin, YANG Nong, CHEN Zheng-le, DING Wen-jun
2010, 16(1): 96-107.
Abstract (218) HTML (93) PDF (399KB)(4)
Abstract:
The Kaladawan area at eastern part of the Altyn Tagh Mountain is tectonically situated between the NE-trending Altyn Tagh strike-slip fault and the W-E-trending Northern Altyn Tagh margin fault. In the area, there appears a set of volcanic-sedimentary rocks. A geochemical study has been made on the ...
3D NUMERICAL SIMULATION OF SLOPE STABILITY OF LANCANGJIANG BRIDGE ON DALI-RUILI RAILWAY
DU Yu-ben, ZHENG Guang, JIANG Liang-wen, XU Qiang
2010, 16(1): 108-114.
Abstract (260) HTML (116) PDF (884KB)(4)
Abstract:
The Lancangjiang Bridge is one of the controlled engineerings on the under-construction Dali-Ruili Railway. Along the bank slopes at which the bridge site is located there are greatly developed long-extending dip-slope joints and nearly vertical joints, The excavation area of the bridge site on righ...

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