Arid
DOI10.1016/j.palaeo.2017.09.023
Genesis of the late Eocene bedded halite in the Qaidam Basin and its implication for paleoclimate in East Asia
Guo, Pei1; Liu, Chiyang1; Huang, Lei1; Wang, Peng2; Wang, Ke2; Yuan, Haili2; Xu, Chongkai1; Zhang, Yiyin1
通讯作者Guo, Pei ; Liu, Chiyang
来源期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
EISSN1872-616X
出版年2017
卷号487页码:364-380
英文摘要

It has long been suggested that the Eocene climate in East Asia was characterized by three latitudinally distributed zones, one middle arid zone and two humid zones to its north and south. The middle arid zone was firstly proposed based on the widespread red beds and evaporites in a NWW-trending zone of China. However, this long-standing model has recently been challenged by increasing doubts about the effectiveness of these arid climate indicators. The Qaidam Basin, as one of the Eocene evaporites-bearing basins in China, can be studied to test whether the bedded evaporites can validly indicate arid climate. Over 300-m halite beds have been found in the late Eocene Upper Xiaganchaigou (UXG) Formation in a local saline center (Shizigou area) of the Qaidam Basin. Its coexistence with source rocks and limited distribution, together with the absence of red beds, make it difficult to explain the halite genesis with the conventional climatic-controlled playa model. Based on strati graphic correlation, lithological and mineralogical observation, and oxygen, carbon and chlorine isotopic analysis, we identify several characteristics about the Shizigou saline center: (1) undulated lake floor; (2) shallow water; (3) limited hydrothermal impact; (4) evaporation-induced precipitation; (5) high eolian influence; and (6) fluctuated climate background. According to these investigations, we suggest a new model for the genesis of the bedded halite in the Qaidam Basin, the tectonic-climatic model. The key point for this model is that the undulated topography caused by tectonic activity and the fluctuated climate together leaded to the hydrological isolation of the Shizigou area. The Shizigou area was isolated from the larger brackish Qaidam paleolake for independent evaporation during arid climate stage while connected with it during humid climate stage, causing alternatively water influx and evaporation and inducing the occurrence of interbedded halite and source rocks. Thus, the widespread bedded halite in the Eocene strata over China may indicate fluctuated rather than arid climate in East Asia.


英文关键词Paleogene Evaporites Chlorine isotopes Fluctuated climate Tibetan plateau
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000414881100030
WOS关键词GREEN RIVER FORMATION ; OLIGOCENE CLIMATE TRANSITION ; IONIZATION MASS-SPECTROMETRY ; NORTHEASTERN TIBETAN PLATEAU ; PICEANCE CREEK BASIN ; STABLE-ISOTOPE ; SALINITY CRISIS ; TECTONIC UPLIFT ; TARIM BASIN ; EBRO BASIN
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS研究方向Physical Geography ; Geology ; Paleontology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/201373
作者单位1.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Shaanxi, Peoples R China;
2.Qinghai Oilfield Co, PetroChina, Dunhuang 736202, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Guo, Pei,Liu, Chiyang,Huang, Lei,et al. Genesis of the late Eocene bedded halite in the Qaidam Basin and its implication for paleoclimate in East Asia[J],2017,487:364-380.
APA Guo, Pei.,Liu, Chiyang.,Huang, Lei.,Wang, Peng.,Wang, Ke.,...&Zhang, Yiyin.(2017).Genesis of the late Eocene bedded halite in the Qaidam Basin and its implication for paleoclimate in East Asia.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,487,364-380.
MLA Guo, Pei,et al."Genesis of the late Eocene bedded halite in the Qaidam Basin and its implication for paleoclimate in East Asia".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 487(2017):364-380.
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