FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4376126905> ?p ?o ?g. }

• W4376126905 endingPage "236" @default.
• W4376126905 startingPage "225" @default.
• W4376126905 abstract "Complex lithofacies of Lucaogou Formation in Jimusar Sag promote strong heterogeneity of oil distribution in fine grained sedimentary rocks. It is of great significance to define the formation mechanism of fine-grained sedimentary rocks for favorable reservoir prediction and exploration target selection in Jimusar Sag. Based on detailed petrographic characterization, in-situ geochemical parameter testing, and high-resolution cycle analysis, sedimentary cycles on the micron to meter scales were successfully identified in Lucaogou Formation from Jimusar Sag. Precession-forced paleo-environmental evolution mainly induces the deposition of meter-scale sedimentary cycles. In the period of low precession, the paleo-environment is cold and dry, the lake level falls. Silt-grained particles advance toward the center of the lake basin carried by gravity current, thus siliciclastic sediments are mainly deposited. In the period of high precession, the climate is warm and humid, the lake level rises. The inputs of siliciclastic sediments are limited and the temperature increases, which are conductive to the carbonate deposition. On this basis, high-frequency paleo-environmental evolution caused by solar activity (70–110yr cycle) further induces the formation of sedimentary cycles on micron-centimeter scale. When the precession is low, the rise and fall of lake level controlled by solar activity is contribute to the deposition of tuff-rich lamina and silt-grained felsic lamina, respectively. The period of high precession is under the background of overall high lake-level, the rise and fall of lake level, along with fall and rise of temperature, controlled by solar activity finally induce the deposition of tuff-rich lamina and carbonate lamina, respectively. The development of multi-scale sedimentary cycles controlled by Milankovitch cycle and solar activity cycle have important implications for shale oil enrichment. The fine-grained sediments deposited during the period of low precession and intense solar activity dominate feldspar dissolution pores and intergranular pores, which are favorable for shale oil enrichment." @default.
• W4376126905 created "2023-05-12" @default.
• W4376126905 creator A5011413537 @default.
• W4376126905 creator A5017100408 @default.
• W4376126905 creator A5028115428 @default.
• W4376126905 creator A5046720090 @default.
• W4376126905 creator A5091922318 @default.
• W4376126905 date "2023-01-01" @default.
• W4376126905 modified "2023-10-01" @default.
• W4376126905 title "Genetic mechanism of multi-scale sedimentary cycles and their impacts on shale-oil distribution in Permian Lucaogou Formation, Jimusar Sag, Junggar Basin" @default.
• W4376126905 cites W1543300520 @default.
• W4376126905 cites W1978461058 @default.
• W4376126905 cites W1980437451 @default.
• W4376126905 cites W1991748626 @default.
• W4376126905 cites W2020985180 @default.
• W4376126905 cites W2025308240 @default.
• W4376126905 cites W2033996162 @default.
• W4376126905 cites W2041591115 @default.
• W4376126905 cites W2046037853 @default.
• W4376126905 cites W2054362988 @default.
• W4376126905 cites W2055527206 @default.
• W4376126905 cites W2057396586 @default.
• W4376126905 cites W2063091092 @default.
• W4376126905 cites W2071250096 @default.
• W4376126905 cites W2082972472 @default.
• W4376126905 cites W2089296274 @default.
• W4376126905 cites W2089400264 @default.
• W4376126905 cites W2116726707 @default.
• W4376126905 cites W2146883564 @default.
• W4376126905 cites W2173623002 @default.
• W4376126905 cites W2382984315 @default.
• W4376126905 cites W2892225831 @default.
• W4376126905 cites W2904390482 @default.
• W4376126905 cites W2915502269 @default.
• W4376126905 cites W2937958085 @default.
• W4376126905 cites W2948412369 @default.
• W4376126905 cites W2954906583 @default.
• W4376126905 cites W2970544755 @default.
• W4376126905 cites W2973072980 @default.
• W4376126905 cites W2997746746 @default.
• W4376126905 cites W3013353288 @default.
• W4376126905 cites W3014842999 @default.
• W4376126905 cites W3101471239 @default.
• W4376126905 cites W3120424230 @default.
• W4376126905 cites W3139409316 @default.
• W4376126905 cites W4200267578 @default.
• W4376126905 cites W4200328819 @default.
• W4376126905 cites W4200384556 @default.
• W4376126905 cites W4223981551 @default.
• W4376126905 cites W4251014520 @default.
• W4376126905 cites W4362581262 @default.
• W4376126905 cites W47157295 @default.
• W4376126905 doi "https://doi.org/10.1016/j.uncres.2023.05.001" @default.
• W4376126905 hasPublicationYear "2023" @default.
• W4376126905 type Work @default.
• W4376126905 citedByCount "0" @default.
• W4376126905 crossrefType "journal-article" @default.
• W4376126905 hasAuthorship W4376126905A5011413537 @default.
• W4376126905 hasAuthorship W4376126905A5017100408 @default.
• W4376126905 hasAuthorship W4376126905A5028115428 @default.
• W4376126905 hasAuthorship W4376126905A5046720090 @default.
• W4376126905 hasAuthorship W4376126905A5091922318 @default.
• W4376126905 hasBestOaLocation W43761269051 @default.
• W4376126905 hasConcept C109007969 @default.
• W4376126905 hasConcept C114793014 @default.
• W4376126905 hasConcept C126753816 @default.
• W4376126905 hasConcept C127313418 @default.
• W4376126905 hasConcept C17409809 @default.
• W4376126905 hasConcept C2776169166 @default.
• W4376126905 hasConcept C6494504 @default.
• W4376126905 hasConcept C93257316 @default.
• W4376126905 hasConceptScore W4376126905C109007969 @default.
• W4376126905 hasConceptScore W4376126905C114793014 @default.
• W4376126905 hasConceptScore W4376126905C126753816 @default.
• W4376126905 hasConceptScore W4376126905C127313418 @default.
• W4376126905 hasConceptScore W4376126905C17409809 @default.
• W4376126905 hasConceptScore W4376126905C2776169166 @default.
• W4376126905 hasConceptScore W4376126905C6494504 @default.
• W4376126905 hasConceptScore W4376126905C93257316 @default.
• W4376126905 hasFunder F4320321001 @default.
• W4376126905 hasFunder F4320327720 @default.
• W4376126905 hasFunder F4320328119 @default.
• W4376126905 hasLocation W43761269051 @default.
• W4376126905 hasOpenAccess W4376126905 @default.
• W4376126905 hasPrimaryLocation W43761269051 @default.
• W4376126905 hasRelatedWork W131025033 @default.
• W4376126905 hasRelatedWork W2030675100 @default.
• W4376126905 hasRelatedWork W2057210365 @default.
• W4376126905 hasRelatedWork W2070515790 @default.
• W4376126905 hasRelatedWork W2167050352 @default.
• W4376126905 hasRelatedWork W2379707404 @default.
• W4376126905 hasRelatedWork W2387551409 @default.
• W4376126905 hasRelatedWork W2967502517 @default.
• W4376126905 hasRelatedWork W3021596666 @default.
• W4376126905 hasRelatedWork W3091832477 @default.
• W4376126905 hasVolume "3" @default.
• W4376126905 isParatext "false" @default.
• W4376126905 isRetracted "false" @default.

• next