@article{MENG2024, 
author = {Xiangzhen MENG and Tiancai DOU and Renhai PU and Xiaoping GAO and Gang LIU and Ming SONG and Yujie FAN},
title = {Changes from south to north in the microfacies of clasticbarrier coastal sandbodies of the Benxi Formation in the Ordos Basin},
year = {2024},
journal = {Journal of Northwest University (Natural Science Edition)},
volume = {54},
number = {3},
pages = {555-568},
keywords = {strong wave barrier, weak wave barrier, shoal, tidal channel, sand body dimensionand distribution},
url = {https://www.sciopen.com/article/10.16152/j.cnki.xdxbzr.2024-03-018},
doi = {10.16152/j.cnki.xdxbzr.2024-03-018},
abstract = {Based on core and thin section observations, as well as statistical analyzes of sandstone thickness and percentage of sandstone content from 1446 wells, we analyzed the coastal changes and control factors of the microfacies type, planar morphology and distribution of the Benxi Fm sandbodies in the Yanchang gas field. The results indicate that the Benxi Fm of the Yanchang gas field is generally composed of terrigenous coastal clastic barrier deposits in a medium to small tidal range environment, but the wave action in the southern region is weak, forming typical barrier sandbars and backbarrier deposits. The wave actions in the north change more strongly, forming three major microfacies sandbodies: reworked barriers, shoals and incised valley filled tidal channels. The barrier sandbodies are arranged in a belt or bead-like pattern parallel to the shoreline and are distributed longshore near the provenance. The oval-shaped shoal sandbodies are dispersed further from the shoreline, and the filling of tidal channel sandbodies is controlled by ancient geomorphic grooves. This research has important guiding significance for the identification and evaluation of reservoirs in the Yanchang gas field and similar geological settings.}
}