FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4312156720> ?p ?o ?g. }

• W4312156720 endingPage "106317" @default.
• W4312156720 startingPage "106317" @default.
• W4312156720 abstract "The sandy conglomerates of the lower member of Shahejie (Es4x) in the north of Dongying Sag, Bohai Bay Basin, were investigated to understand the formation mechanism of the good reservoir and controlling factors in deeply buried strata. This research is based on seismic, logging, and core data and comprehensively utilizes methods such as core description, petrographic analysis, cathodoluminescence image analysis, SEM-EDS analysis, and mercury intrusion. The sandy conglomerates are predominantly lithic arkose and litharenite. The reservoirs in the Es4x have experienced three diagenetic processes, compaction, dissolution, and cementation. Compaction remains the major factor affecting the reservoir quality, mainly in the progradation sequence, and cementation has a destructive effect on reservoirs, principally in the retrogradation sequence. The quantification of the compaction by the compaction index revealed that mechanical compaction is higher in the progradation sequence (0.68) than in the retrogradation sequences (0.59). Compaction is suppressed by carbonate cementation, but the extensive cementation significantly degrades the reservoir quality, especially in the retrogradation sequence. Dissolution of different rock fragments, feldspar, and the whole dissolution, in general, enhance the reservoir's quality in both intervals but more in the progradation sequence. Three types of reservoirs representing type I, type II, and Type III mercury intrusion capillary pressure curves were encountered in the Es4x. The braided channels in the progradation and retrogradation sets encompass the greatest reservoir quality and are characterized by type I and II reservoirs with good petrophysical properties. The preeminent reservoirs appear in the braided channels of the progradation set. The development of high-quality reservoirs is governed by the depositional subfacies, compaction, and dissolution in the Es4x. This study will contribute to comprehending the origin of the genesis mechanism of high-quality in deep sublacustrine sandy conglomerate and will help the exploration and pre-drill for favorable reservoirs in similar basins around the world." @default.
• W4312156720 created "2023-01-04" @default.
• W4312156720 creator A5005380192 @default.
• W4312156720 creator A5006452592 @default.
• W4312156720 creator A5009722101 @default.
• W4312156720 creator A5013277954 @default.
• W4312156720 creator A5025247932 @default.
• W4312156720 creator A5041230530 @default.
• W4312156720 creator A5088797400 @default.
• W4312156720 date "2023-02-01" @default.
• W4312156720 modified "2023-09-25" @default.
• W4312156720 title "Impact of sedimentation and diagenesis on deeply buried sandy conglomerate reservoirs quality in nearshore sublacustrine fan: A case study of lower Member of the Eocene Shahejie Formation in Dongying Sag, Bohai Bay Basin (East China)" @default.
• W4312156720 cites W1849879787 @default.
• W4312156720 cites W1989114823 @default.
• W4312156720 cites W1996737977 @default.
• W4312156720 cites W2020415754 @default.
• W4312156720 cites W2021765498 @default.
• W4312156720 cites W2031952526 @default.
• W4312156720 cites W2036629887 @default.
• W4312156720 cites W2040650331 @default.
• W4312156720 cites W2047905521 @default.
• W4312156720 cites W2065559873 @default.
• W4312156720 cites W2074536715 @default.
• W4312156720 cites W2077673579 @default.
• W4312156720 cites W2126963790 @default.
• W4312156720 cites W2130135197 @default.
• W4312156720 cites W2138821921 @default.
• W4312156720 cites W2141786559 @default.
• W4312156720 cites W2142006672 @default.
• W4312156720 cites W2151557469 @default.
• W4312156720 cites W2178038374 @default.
• W4312156720 cites W2180740776 @default.
• W4312156720 cites W2212528985 @default.
• W4312156720 cites W2489797200 @default.
• W4312156720 cites W2548576269 @default.
• W4312156720 cites W2550390687 @default.
• W4312156720 cites W2554996062 @default.
• W4312156720 cites W2585033147 @default.
• W4312156720 cites W2588427413 @default.
• W4312156720 cites W2591501153 @default.
• W4312156720 cites W2606517370 @default.
• W4312156720 cites W2612417264 @default.
• W4312156720 cites W2612542741 @default.
• W4312156720 cites W2741560269 @default.
• W4312156720 cites W2789267055 @default.
• W4312156720 cites W2792031555 @default.
• W4312156720 cites W2793511398 @default.
• W4312156720 cites W2884502747 @default.
• W4312156720 cites W2887710329 @default.
• W4312156720 cites W2888541958 @default.
• W4312156720 cites W2900616946 @default.
• W4312156720 cites W2921859655 @default.
• W4312156720 cites W2938440248 @default.
• W4312156720 cites W2944055699 @default.
• W4312156720 cites W2968757044 @default.
• W4312156720 cites W2976215816 @default.
• W4312156720 cites W2976709196 @default.
• W4312156720 cites W2994434476 @default.
• W4312156720 cites W3005475908 @default.
• W4312156720 cites W3014619985 @default.
• W4312156720 cites W3015169375 @default.
• W4312156720 cites W3021535020 @default.
• W4312156720 cites W3027323540 @default.
• W4312156720 cites W3038550927 @default.
• W4312156720 cites W3039787259 @default.
• W4312156720 cites W3087374930 @default.
• W4312156720 cites W3090060585 @default.
• W4312156720 cites W3095038345 @default.
• W4312156720 cites W3149917015 @default.
• W4312156720 cites W3158966884 @default.
• W4312156720 cites W3162314681 @default.
• W4312156720 cites W3181895832 @default.
• W4312156720 cites W3196774976 @default.
• W4312156720 cites W3197874779 @default.
• W4312156720 cites W3217203725 @default.
• W4312156720 cites W4292230017 @default.
• W4312156720 doi "https://doi.org/10.1016/j.sedgeo.2022.106317" @default.
• W4312156720 hasPublicationYear "2023" @default.
• W4312156720 type Work @default.
• W4312156720 citedByCount "0" @default.
• W4312156720 crossrefType "journal-article" @default.
• W4312156720 hasAuthorship W4312156720A5005380192 @default.
• W4312156720 hasAuthorship W4312156720A5006452592 @default.
• W4312156720 hasAuthorship W4312156720A5009722101 @default.
• W4312156720 hasAuthorship W4312156720A5013277954 @default.
• W4312156720 hasAuthorship W4312156720A5025247932 @default.
• W4312156720 hasAuthorship W4312156720A5041230530 @default.
• W4312156720 hasAuthorship W4312156720A5088797400 @default.
• W4312156720 hasConcept C109007969 @default.
• W4312156720 hasConcept C114793014 @default.
• W4312156720 hasConcept C126753816 @default.
• W4312156720 hasConcept C127313418 @default.
• W4312156720 hasConcept C130452526 @default.
• W4312156720 hasConcept C146588470 @default.
• W4312156720 hasConcept C16565575 @default.
• W4312156720 hasConcept C166957645 @default.
• W4312156720 hasConcept C17409809 @default.
• W4312156720 hasConcept C185592680 @default.

• next