Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China

Based on core data, thin section and logging, this study investigates the basic characteristics and occurrence regularities of the Ordovician buried-hill carbonate reservoir in the Bozhong 21-2 tectonic belt. Results show that the reservoir lithology is primarily limestone, followed by dolomite, dol...

Full description

Saved in:
Bibliographic Details
Published in:Petroleum science and technology 2018-09, Vol.36 (17), p.1374-1381
Main Authors: Ren, ChangQing, Gao, XianZhi, Jiang, Haishen, Li, JiuMei, He, FuGui
Format: Article
Language:English
Subjects:
Bozhong 21-2 tectonic belt
carbonate
karstification
Ordovician
reservoir space
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393
cites cdi_FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393
container_end_page 1381
container_issue 17
container_start_page 1374
container_title Petroleum science and technology
container_volume 36
creator Ren, ChangQing
Gao, XianZhi
Jiang, Haishen
Li, JiuMei
He, FuGui
description Based on core data, thin section and logging, this study investigates the basic characteristics and occurrence regularities of the Ordovician buried-hill carbonate reservoir in the Bozhong 21-2 tectonic belt. Results show that the reservoir lithology is primarily limestone, followed by dolomite, dolomitic limestone or limey dolomite, and silty mudstone. The reservoir spaces are primarily composed of secondary porosity. These reservoirs can be divided vertically into weathered-crust karst reservoirs and inner dissolution-type reservoirs. The distribution of reservoirs is controlled chiefly by karstification. The high karst units in the study area are favorable for the development of the two reservoir types.
doi_str_mv 10.1080/10916466.2018.1474222
format article
fullrecord <record><control><sourceid>crossref_infor</sourceid><recordid>TN_cdi_crossref_primary_10_1080_10916466_2018_1474222</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>10_1080_10916466_2018_1474222</sourcerecordid><originalsourceid>FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393</originalsourceid><addsrcrecordid>eNp9kM1u1EAQhC0UJJLAIyD1A8TL9NjjtW9JVgkgrZQLnK32_OBGzkzUMyzaPAjPi1cJVw6lLqmr6vBV1UdUG1S9-oRqwK7tuo1W2G-w3bZa6zfVOZpG17o1w9nq10x9Cr2rLnL-qRQOW-zOqz-7mYRs8cK5sM1A0UGgQxKaFg8knuBJvGNbOEVIAR7EpQNbpgjTL2Hv6pmXBSzJlCIVD-Kzl0NiycARyuzhNj3PKf4AjbWG4m1JkS1MfilX628mhls6rsocr2A3c6T31dtAS_YfXu9l9f3-7tvuS71_-Px1d7OvbYOq1L226DRpo40ZBgyT0VOHHo3ZtkQWtZv6VoUe-8Y2NqhBeae1C32Pxk_N0FxW5mXXSspZfBifhB9JjiOq8QR3_Ad3PMEdX-GuveuXHseQ5JF-J1ncWOi4JAlC0XIem_9P_AXMBoIj</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China</title><source>Taylor and Francis Science and Technology Collection</source><creator>Ren, ChangQing ; Gao, XianZhi ; Jiang, Haishen ; Li, JiuMei ; He, FuGui</creator><creatorcontrib>Ren, ChangQing ; Gao, XianZhi ; Jiang, Haishen ; Li, JiuMei ; He, FuGui</creatorcontrib><description>Based on core data, thin section and logging, this study investigates the basic characteristics and occurrence regularities of the Ordovician buried-hill carbonate reservoir in the Bozhong 21-2 tectonic belt. Results show that the reservoir lithology is primarily limestone, followed by dolomite, dolomitic limestone or limey dolomite, and silty mudstone. The reservoir spaces are primarily composed of secondary porosity. These reservoirs can be divided vertically into weathered-crust karst reservoirs and inner dissolution-type reservoirs. The distribution of reservoirs is controlled chiefly by karstification. The high karst units in the study area are favorable for the development of the two reservoir types.</description><identifier>ISSN: 1091-6466</identifier><identifier>EISSN: 1532-2459</identifier><identifier>DOI: 10.1080/10916466.2018.1474222</identifier><language>eng</language><publisher>Taylor &amp; Francis</publisher><subject>Bozhong 21-2 tectonic belt ; carbonate ; karstification ; Ordovician ; reservoir space</subject><ispartof>Petroleum science and technology, 2018-09, Vol.36 (17), p.1374-1381</ispartof><rights>2018 Taylor &amp; Francis Group, LLC 2018</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393</citedby><cites>FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Ren, ChangQing</creatorcontrib><creatorcontrib>Gao, XianZhi</creatorcontrib><creatorcontrib>Jiang, Haishen</creatorcontrib><creatorcontrib>Li, JiuMei</creatorcontrib><creatorcontrib>He, FuGui</creatorcontrib><title>Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China</title><title>Petroleum science and technology</title><description>Based on core data, thin section and logging, this study investigates the basic characteristics and occurrence regularities of the Ordovician buried-hill carbonate reservoir in the Bozhong 21-2 tectonic belt. Results show that the reservoir lithology is primarily limestone, followed by dolomite, dolomitic limestone or limey dolomite, and silty mudstone. The reservoir spaces are primarily composed of secondary porosity. These reservoirs can be divided vertically into weathered-crust karst reservoirs and inner dissolution-type reservoirs. The distribution of reservoirs is controlled chiefly by karstification. The high karst units in the study area are favorable for the development of the two reservoir types.</description><subject>Bozhong 21-2 tectonic belt</subject><subject>carbonate</subject><subject>karstification</subject><subject>Ordovician</subject><subject>reservoir space</subject><issn>1091-6466</issn><issn>1532-2459</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp9kM1u1EAQhC0UJJLAIyD1A8TL9NjjtW9JVgkgrZQLnK32_OBGzkzUMyzaPAjPi1cJVw6lLqmr6vBV1UdUG1S9-oRqwK7tuo1W2G-w3bZa6zfVOZpG17o1w9nq10x9Cr2rLnL-qRQOW-zOqz-7mYRs8cK5sM1A0UGgQxKaFg8knuBJvGNbOEVIAR7EpQNbpgjTL2Hv6pmXBSzJlCIVD-Kzl0NiycARyuzhNj3PKf4AjbWG4m1JkS1MfilX628mhls6rsocr2A3c6T31dtAS_YfXu9l9f3-7tvuS71_-Px1d7OvbYOq1L226DRpo40ZBgyT0VOHHo3ZtkQWtZv6VoUe-8Y2NqhBeae1C32Pxk_N0FxW5mXXSspZfBifhB9JjiOq8QR3_Ad3PMEdX-GuveuXHseQ5JF-J1ncWOi4JAlC0XIem_9P_AXMBoIj</recordid><startdate>20180902</startdate><enddate>20180902</enddate><creator>Ren, ChangQing</creator><creator>Gao, XianZhi</creator><creator>Jiang, Haishen</creator><creator>Li, JiuMei</creator><creator>He, FuGui</creator><general>Taylor &amp; Francis</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20180902</creationdate><title>Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China</title><author>Ren, ChangQing ; Gao, XianZhi ; Jiang, Haishen ; Li, JiuMei ; He, FuGui</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Bozhong 21-2 tectonic belt</topic><topic>carbonate</topic><topic>karstification</topic><topic>Ordovician</topic><topic>reservoir space</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ren, ChangQing</creatorcontrib><creatorcontrib>Gao, XianZhi</creatorcontrib><creatorcontrib>Jiang, Haishen</creatorcontrib><creatorcontrib>Li, JiuMei</creatorcontrib><creatorcontrib>He, FuGui</creatorcontrib><collection>CrossRef</collection><jtitle>Petroleum science and technology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ren, ChangQing</au><au>Gao, XianZhi</au><au>Jiang, Haishen</au><au>Li, JiuMei</au><au>He, FuGui</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China</atitle><jtitle>Petroleum science and technology</jtitle><date>2018-09-02</date><risdate>2018</risdate><volume>36</volume><issue>17</issue><spage>1374</spage><epage>1381</epage><pages>1374-1381</pages><issn>1091-6466</issn><eissn>1532-2459</eissn><abstract>Based on core data, thin section and logging, this study investigates the basic characteristics and occurrence regularities of the Ordovician buried-hill carbonate reservoir in the Bozhong 21-2 tectonic belt. Results show that the reservoir lithology is primarily limestone, followed by dolomite, dolomitic limestone or limey dolomite, and silty mudstone. The reservoir spaces are primarily composed of secondary porosity. These reservoirs can be divided vertically into weathered-crust karst reservoirs and inner dissolution-type reservoirs. The distribution of reservoirs is controlled chiefly by karstification. The high karst units in the study area are favorable for the development of the two reservoir types.</abstract><pub>Taylor &amp; Francis</pub><doi>10.1080/10916466.2018.1474222</doi><tpages>8</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1091-6466
ispartof Petroleum science and technology, 2018-09, Vol.36 (17), p.1374-1381
issn 1091-6466
1532-2459
language eng
recordid cdi_crossref_primary_10_1080_10916466_2018_1474222
source Taylor and Francis Science and Technology Collection
subjects Bozhong 21-2 tectonic belt
carbonate
karstification
Ordovician
reservoir space
title Characteristics and favorable area prediction of Ordovician buried-hill carbonate reservoirs in the Bozhong 21-2 tectonic belt, Bohai Bay Basin, China
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-01T01%3A42%3A24IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-crossref_infor&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Characteristics%20and%20favorable%20area%20prediction%20of%20Ordovician%20buried-hill%20carbonate%20reservoirs%20in%20the%20Bozhong%2021-2%20tectonic%20belt,%20Bohai%20Bay%20Basin,%20China&rft.jtitle=Petroleum%20science%20and%20technology&rft.au=Ren,%20ChangQing&rft.date=2018-09-02&rft.volume=36&rft.issue=17&rft.spage=1374&rft.epage=1381&rft.pages=1374-1381&rft.issn=1091-6466&rft.eissn=1532-2459&rft_id=info:doi/10.1080/10916466.2018.1474222&rft_dat=%3Ccrossref_infor%3E10_1080_10916466_2018_1474222%3C/crossref_infor%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c310t-82c1d2a25255991fb52b61e15574aac12db840f8183c3cf090ed22df8815eb393%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true