Whole-Rock Geochemistry and Mineralogy of Triassic Montney Formation, Northeastern British Columbia, Western Canada Sedimentary Basin
Whole-Rock Geochemistry and Mineralogy of Triassic Montney Formation, Northeastern British Columbia, Western Canada Sedimentary Basin作者机构:Department of Earth and Atmospheric Sciences University of Alberta Edmonton Canada
出 版 物:《International Journal of Geosciences》 (地球科学国际期刊(英文))
年 卷 期:2016年第7卷第1期
页 面:91-114页
学科分类:081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程]
主 题:Geochemistry Whole-Rock Mineralogy Montney Formation Thin-Section Petrography Trace-Elements ICP-MS XRD Dolomitization Diagenesis WCSB
摘 要:Inductively Coupled Plasma-Mass Spectrometry (ICP-MS)was used to analyze chemical elements—major, trace and rare earth elements(REE) concentrations, augmented with quantitative X-ray diffraction (XRD) analysis and thin-section petrography formineralogical characterization of the Triassic Montney Formation in northeastern British Columbia, Western Canada SedimentaryBasin (WCSB). Results from this study indicatethat integration of chemical elements with mineralogy shows affinity to the host lithologies. Evidently, chemical elements are the building blocks for minerals, thus, their significancesin the interpretation of geological systems are unambiguous. Herein, major elements concentration such as Al, Fe, K, Mg, Ca, Mn in the samples analyzed from the Montney Formation are interpreted as: 1) indication of dolomitization and diagenesis;2) trace elements—Rb, Th, U, and Cs are related to the organi