Advances in Engineering Research, volume 94 2nd International Conference on Sustainable Development (ICSD 2016) Paleoenvironment of Carboniferous Shales in Wuwei Basin Hui-yu HAN Zhi-hong KANG* School of Energy Resources, CUGB School of Energy Resources, CUGB China University of Geosciences, Beijing China University of Geosciences, Beijing Beijing, China Beijing, China e-mail:
[email protected] e-mail: 250586274 @qq.com Yuan-yuan PENG Lei ZHOU School of Energy Resources, CUGB School of Energy Resources, CUGB China University of Geosciences, Beijing China University of Geosciences, Beijing Beijing, China Beijing, China e-mail: 854946290 @qq.com e-mail: 755302856 @qq.com Abstract—Shales are enriched with diverse suites of trace inductively coupled plasma mass spectrometry (GB / T elements that reflect their depositional environment. The 14506.30-2010). Samples were analyzed by Analtical purpose of this paper is to restitute the paleoenvironment of Laboratory of Beijing Research Institute of Uranium Carboniferous shales in Wuwei basin. In this study, we used Geology. Test results were shown in Table 1: and analyzed comprehensively trace elements(B, Sr, Ba, Ga, V, Ni, Co, U, Th) data of shales. We resulted that shales for III. METHODS Carboniferous from the southern margin of the Wuwei basin The contents of trace elements in sediments are closely were deposited in the hot and salty marine-continental transition environment. related to the salinity, redox conditions, climate and water depth of sediment’sdepositional environment.In order to Keywords-shales;paleoenvironment; trace elements restore the sedimentary environment accurately, this paper analyzed the sedimentary environment of Carboniferous I. INTRODUCTION shales in Wuwei Basin from three aspects.