检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:Mohammad Abdelfattah Sarhan
机构地区:[1]Geology Department,Faculty of Science,Damietta University,New Damietta City,34517,Egypt
出 处:《Petroleum Research》2022年第4期511-520,共10页石油研究(英文)
摘 要:The tectonic deformation has a significant influence on the hydrocarbon reservoirs properties.The effect of this process focuses on the lateral distribution of the petrophysical parameters characterizing the hydrocarbon reservoirs.The main objective of the current study is to perform a petrophysical examination of the Abu Madi gas reservoir which is the greatest gas-bearing reservoir at Nile Delta Basin in order to examine how far the Messinian tectonics affected the lateral variations of these petrophysical parameters.This petrophysical evaluation was performed based on the wireline log data acquired for five wells,namely,Abu Madi-2,Abu Madi-7,El Qara-3,Nidoco-7,and Nidoco-9 drilled within the Abu Madi Paleo-Valley.The petrophysical assessment for the most promising zone intervals within the Abu Madi sandstones in the inspected wells show that the total porosity varies between 17%and 22%,the effective porosity ranges from 7%to 19%,the shale volume fluctuates between 16%and 30%,hydrocarbon satu-ration varies from 37%to 76%,and the bulk volume of water varies between 0.02 and 0.09.These significant variations in the petrophysical properties of the Abu Madi reservoir are attributed to the tectonic influence during the deposition of the Abu Madi Formation as a part of the Late Miocene synrift megasequence in the Nile Delta Basin.This conclusion confirms that the petrophysical properties of sandstone reservoirs are function of tectonic and structural deformation.
关 键 词:Abu madi formation Messinian reservoir Nile delta basin Petrophysical parameters Well logging
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.210