Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?

被引：1

作者：

LAI Zhongping

机构：

[1] Key Laboratory of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences

[2] State Key Laboratory of Cryosphere Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences

来源：

Acta Geologica Sinica(English Edition) | 2014年 / S1期

关键词：

Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary; OSL;

D O I：

暂无

中图分类号：

P534.63 [第四纪（系）];

学科分类号：

070905 ;

摘要：

A geological feature in the Qaidam Basin known as the"Shell Bar"contains millions of freshwater articulated clam shells buried in-situ.Since the 1980s this feature in the now hyper-arid basin has been interpreted to be lake deposits that provide evidence for a warmer and more humid climate than present during late Marine Isotope Stage 3(MIS 3)(Bowler et al.,1986).However,the global climate during

引用

页码：14 / 14

页数：1

共 50 条

[1] Was the enclosed Qaidam Basin of The Tibetan Plateau Accumulative or Erosive during the Late Quaternary?
LAI Zhongping
[J]. ActaGeologicaSinica(EnglishEdition), 2014, 88(S1) (EnglishEdition) : 14
[2] Reduced chemical weathering intensity in the Qaidam Basin (NE Tibetan Plateau) during the Late Cenozoic
Bao, Jing
Song, Chunhui
Yang, Yibo
Fang, Xiaomin
Meng, Qingquan
Feng, Ying
He, Pengju
[J]. JOURNAL OF ASIAN EARTH SCIENCES, 2019, 170 : 155 - 165
[3] Late Holocene vegetation and climate oscillations in the Qaidam Basin of the northeastern Tibetan Plateau
Zhao, Yan
Yu, Zicheng
Liu, Xiuju
Zhao, Cheng
Chen, Fahu
Zhang, Ke
[J]. QUATERNARY RESEARCH, 2010, 73 (01) : 59 - 69
[4] Why Qaidam Basin is amalgamated into Tibetan Plateau but Tarim Basin is not?
Pei Xu
Huangfu PengPeng
Li ZhongHai
Shi YaoLin
[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2022, 65 (11): : 4259 - 4272
[5] On the nature of the ice cap on the Tibetan Plateau during the late Quaternary
Gupta, S. K.
Sharma, P.
[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 1992, 97 (04) : 339 - 343
[6] Dry periods on the NE Tibetan Plateau during the late Quaternary
Ijmker, Janneke
Stauch, Georg
Poetsch, Steffen
Diekmann, Bernhard
Wuennemann, Bernd
Lehmkuhl, Frank
[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2012, 346 : 108 - 119
[7] Landscape and climate on the northern Tibetan Plateau during the late Quaternary
Stauch, G.
Schulte, P.
Ramisch, A.
Hartmann, K.
Huelle, D.
Lockot, G.
Diekmann, B.
Nottebaum, V.
Mueller, C.
Wuennemann, B.
Yan, D.
Lehmkuhl, F.
[J]. GEOMORPHOLOGY, 2017, 286 : 78 - 92
[8] ON THE NATURE OF THE ICE CAP ON THE TIBETAN PLATEAU DURING THE LATE QUATERNARY
GUPTA, SK
SHARMA, P
[J]. GLOBAL AND PLANETARY CHANGE, 1992, 97 (04) : 339 - 343
[9] Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau
Zhang, Weilin
Li, Tao
Fang, Xiaomin
Zhang, Tao
Yan, Maodu
Zan, Jinbo
Yang, Yibo
Khatri, Dhan Bahadur
[J]. QUATERNARY RESEARCH, 2021, 104 : 170 - 181
[10] Edaphic characterization and plant zonation in the Qaidam Basin, Tibetan Plateau
Xianjie Wang
Fanjing Kong
Weigang Kong
Wenning Xu
[J]. Scientific Reports, 8

← 1 2 3 4 5 →