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《Quaternary Sciences》 2004-01
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THE NEW DATA OF THE UPLIFTING OF QINLING MOUNTAINS SINCE THE MIDDLE PLEISTOCENE

Xue Xiangxu ①② Li Huhou ① Li Yongxiang ① Liu Hujun ①③ (①Key Laboratory of Continental Dynamics, Ministry of Education and Institute of Cenozoic Geology and Environment, Northwest University, Xi′an 710069; ②Institute of Earth Environment, State Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences, Xi′an 710075;③College of Tourism and Environment Science, Shaanxi Normal; University, Xi′an 710062)  
A group of caves, having developed in the strata of Cambrian dolomite limestone and being present in about six different altitudes, were found in the northern part of Qinling Mountains. They are situated at the hill slope behind Zhangping Village being on the left bank of South Luohe River, Luonan County, Shaanxi Province. All the caves were excavated in the past by the local farmers, but there are still more or less undisturbed sediments preserved. A serious of undisturbed fluvial sediment samples in the caves have been collected for dating by the method of selected frequency optical luminescene (SFOL). The results of the dating of the cave group, from the highest, the sixth level, downwards to the lowest, the first level, are: No.6, 0.493±0.055MaB.P.; No.4, 0.259±0.023MaB.P.; No.3, 0.205±0.019MaB.P.;?No.2,?0.031± 0.0 035MaB.P . and the No. 1, 0.028±0.0 032MaB.P. A lot of mammalian fossils (10 gen. and sp. of macro mammals and 28 gen. 23 sp. of micro ones) were collected from the same deposits of these caves. The fossils from the highest cave are Blarinella quadroticauda、Microtus oeconomus、Niviventer confucianus、Rhizomys troglodytes、Hystrix and some genera of lizard of reptile. Most of these fossils appeared also in the deposits of localities such as Loc.1 of Zhou koudian near Beijing, Loc. of Hexian Ape Man in Anhui and Xishuidong of Lantian, Shaanxi. The ages of these localities are almost all in the Middle Pleistocene. In other words, the earlier deposits of the 6th level cave of Zhangping were deposited in the Middle Pleistocene, same as that of Loc.1 of Zhoukoudian, Hexian and Xishuidong. For comparing the age of these six level cave deposits with that of the terraces of Luohe River, the authors investigated the characteristics of Luohe River terraces near the caves of Zhangping area, measured their height and collected samples of the terrace deposits for dating. The age of terrace Ⅲ which is almost at the same altitude of cave 6 or at the height range from 5th to 6th cave, is 0.526±0.051MaB.P. The terrace Ⅱ, same as cave 3 in altitude or at the height range from 3rd to 4th cave, is 0 241±0 025MaB.P. The data of the altitude and the age of both the caves and terraces can be well correlated (Tab.1) . From these, we have obtained an uplifting curve of Qinling Mountains since the Middle Pleistocene (Fig.3). From Fig.3, we may understand that the uplifting rate of Qinling Mountains since the Middle Pleistocene(about 0.5MaB.P.) has fluctuated. And the later the period, the bigger was the uplifting rate, especially since the later part of the Middle Pleistocene. It is almost consistent with the uplifting of the Qinghai Xizang Plateau. It shows that the uplifting of the Qinling Mountains is closely related with that of the Qinghai Xizang Plateau. Only the uplifting height and rate is lower and slower than that of the Qinghai Xizang Plateau, because the Qinghai Xizang Plateau is the main or center area of the uplifting.
【Fund】: 陕西省科学技术委员会;; 陕西省教育委员会基金项目 (批准号 :JK0 2 8和JK0 1);; 中国科学院黄土与第四纪地质国家重点实验室开放基金项目 (SKILQG0 2 19)资助
【CateGory Index】: P534
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Chinese Journal Full-text Database 10 Hits
1 Shi Yafeng; Zheng Benxing; Li Shijie and Ye Baisheng(Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, 730000);Studies on Altitude and Climatic Environment in the Middle and East Parts of Tibetan Plateau during Quaternary Maximum Glaciation[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1995-02
2 WANG SUNG, LU CHANG-KWUN, KAO YLEH-TING, Loo TAI-CHUN(Institute of Zoology, Academia Sinica, Peking);ON THE MAMMALS FROM SOUTHWESTERN KWANGSI, CHINA[J];Acta Zoologica Sinica;1962-04
3 Xu Qin-qi;General trend of the development of the Quaternary stratigraphy——using the study of Lantian Quaternary stratigraphy as example[J];Journal of Stratigraphy;1990-01
4 Teng Zhihong; Shen Xiping(Department of Geology, Northwest (Design Room, Tap Water Company University, Xi'an, 710069) of Xi'an, Xi'an, 710069);A study of eolian loess and its lower boundary in China[J];JOURNAL OF STRATIGRAPHY;1995-02
5 Zhang Guowei Liu Xiaoming (Department of Geology, Northwest University, Xi'an710069);SOME REMARKS ON CHINA CENTRAL OROGENIC SYSTEM[J];;1998-05
6 Dong Xuebin Wang ZhongminTan Chengze Yang HuixinCheng Liren Zhou Yaoxiu Changchun College of Geology. Chinese University of Gcllogy(Beijing). Center of Acrogeophysical Remote Sensing, Ministry of Geology and Mineral Resources.;NEW PALEOMAGNETIC RESULTS FROM YADONG- GOLMUD GEOSCIENCE TRANSECT AND A PRELIMINARY STUDY ON THE MODEL OF TERRANES EVOLUTION IN QINGHAI-XIZANG PLATEAU[J];;1990-02
7 Li Tingdong(The Chinese Academy of Geological Sciences);The Uplifting Process and Mechanism of the Qinhai-Tibet Plateau[J];;1995-01
8 Ding Zhongli; Sun Jimin; Yang Shiling; Xiong ShangfaGu Zhaoyan; Liu Tungsheng(Institute of Geology, Chinese Academy of Sciences, Beijing 100029)Zhu Rixiang; Guo Bin(Institute of Geophysics, Chinese Academy of Sciences, Beijing 100101)Yue Leping(Department;MAGNETOSTRATIGRAPHY AND GRAIN SIZE RECORD OF A THICK RED CLAY-LOESS SEQUENCE AT LINGTAI, THE CHINESE LOESS PLATEAU[J];QUATERNARY SCIENCES;1998-01
9 Ding Zhongli\ Sun Jimin (Institute of Geology,Chinese Academy of Sciences,Beijing\ 100029) Zhu Rixiang\ Guo Bin (Institute of Geophysics,Chinese Academy of Sciences,Beijing\ 100101);EOLIAN ORIGIN OF THE RED CLAY DEPOSITS IN THE LOESS PLATEAU AND IMPLICATIONS FOR PLIOCENE CLIMATIC CHANGES[J];QUATERNARY SCIENCES;1997-02
10 Wu Jiayan Li Guihui (Institute of Zoology, Shanxi);A REPORT ON THE MAMMALS OF ANKANG REGION, SHANXI PROVINCE[J];Zoological Research;1982-01
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