Sandstone grain size characteristics of the Upper Jurassic Emuerhe Formation in the western region, Mohe Basin (NE China). (7th April 2015)

• Record Type: Journal Article
• Authors: Zhang, Ming Ming; Liu, Zhao Jun; Fang, Shi
• Is Part Of: Geological journal. Volume 51:Number 4(2016)
• Page Start: 652
• Page End: 669
• Publication Date: 2015-04-07
• Subjects: Mohe Basin -- Upper Jurassic -- Emuerhe Formation -- sandstone grain size -- hydrodynamic conditions; Geology -- Periodicals; 551
• DOI: 10.1002/gj.2672
• Languages: English
• ISSNs: 0072-1050

Abstract

Abstract : The Upper Jurassic Emuerhe Formation was developed with abundant sedimentary facies types in the western section of the Mohe Basin. Based on the systematic sampling and detailed observation on the Emuerhe Formation of this section, the research on the sandstone grain size characteristics of the Emuerhe Formation was carried out with the grain size parameters features (Mz, SK1, K G and σ 1 ), the sensitive components parameters features (SCPGS, SCGSR and SCPV) and the grain size analytical graphs features (grain size frequency curves, grain size cumulative curves, probability cumulative curves and C–M plots). The comprehensive analytical results illustrate that the hydrodynamic energy of the Emuerhe Formation (three times fan delta facies, two times sandy shallow lake microfacies and five times turbidite deposit) in the western section gradually reduced from bottom to top. In addition, the hydrodynamic energy of each fan delta facies gradually enhanced from bottom to top. Based on the analysis of the hydrodynamic conditions of the Emuerhe Formation in the western section, the hydrodynamic conditions evolution history of this section can be divided into five sedimentary phases, namely respectively for the fan delta sedimentary phase, the first‐time sandy shallow lake microfacies sedimentary phase, the short‐term deep lake subfacies sedimentary phase, the second‐time sandy shallow lake microfacies sedimentary phase and the relatively stable deep lake subfacies sedimentary phase from bottom to top. Copyright © 2015 John Wiley & Sons, Ltd.