FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012509197> ?p ?o ?g. }

• W2012509197 endingPage "247" @default.
• W2012509197 startingPage "234" @default.
• W2012509197 abstract "Abstract An igneous hydrocarbon reservoir had been found in the Z hanhua depression, B ohai B ay B asin, eastern C hina. Two doleritic sills successively intruded into the immature source rock of the third member of the S hahejie F ormation ( Es3 ). The heat released from the magma changed the mineral composition of wall rocks and accelerated the maturity of organic matter. Thin hornfels and carbargilite zones were found next to the sills. The vitrinite reflectances (% R o ) of these heated wall rocks increased to at least 1.4% near the contacts (<50 m), and accumulation of oil was found in the hornfels zone and dolerite bodies. With the aim of understanding the influence of the sills on the hydrocarbon generation process, a complex heat conduction model was used to simulate the thermal history of the organic‐rich wall rocks, in which both the latent heat of crystallization of intrusions and vapourization heat of pore water in wall rocks were considered. The simulation results suggested that the cooling of each sill continued for about 0.1 Ma after its emplacement and the temperature of wall rocks was considerably raised. The peak temperature ( T peak ) that wall rocks experienced can reach 460–650°C in the region of 10 m away from the contacts. The thermal model was qualitatively verified by comparing the experimental data of vitrinite reflectances and mineral geothermometers of the wall rocks with the simulation results. Furthermore, we modelled the hydrocarbon generation of the source rocks based on the simulated thermal history. In the region of about 100 m from the contacts, the organic matter was heated and partially transformed into hydrocarbon within only a few 1000 years, which was significantly faster than the normal burial generation process." @default.
• W2012509197 created "2016-06-24" @default.
• W2012509197 creator A5003572460 @default.
• W2012509197 creator A5004788351 @default.
• W2012509197 creator A5012673624 @default.
• W2012509197 creator A5016576526 @default.
• W2012509197 creator A5041988337 @default.
• W2012509197 creator A5050252452 @default.
• W2012509197 creator A5076031922 @default.
• W2012509197 creator A5085648951 @default.
• W2012509197 date "2011-07-20" @default.
• W2012509197 modified "2023-10-14" @default.
• W2012509197 title "Numerical modelling of the hydrocarbon generation of <scp>T</scp>ertiary source rocks intruded by doleritic sills in the <scp>Z</scp>hanhua depression, <scp>B</scp>ohai <scp>B</scp>ay <scp>B</scp>asin, <scp>C</scp>hina" @default.
• W2012509197 cites W1572315910 @default.
• W2012509197 cites W1617126672 @default.
• W2012509197 cites W1964286025 @default.
• W2012509197 cites W1968142418 @default.
• W2012509197 cites W1969575081 @default.
• W2012509197 cites W1980959253 @default.
• W2012509197 cites W1986457294 @default.
• W2012509197 cites W1997465679 @default.
• W2012509197 cites W1998704123 @default.
• W2012509197 cites W2001936384 @default.
• W2012509197 cites W2003394352 @default.
• W2012509197 cites W2004761050 @default.
• W2012509197 cites W2011146756 @default.
• W2012509197 cites W2017368933 @default.
• W2012509197 cites W2021025164 @default.
• W2012509197 cites W2023867565 @default.
• W2012509197 cites W2029949312 @default.
• W2012509197 cites W2037840723 @default.
• W2012509197 cites W2040073460 @default.
• W2012509197 cites W2042131939 @default.
• W2012509197 cites W2046099038 @default.
• W2012509197 cites W2048032597 @default.
• W2012509197 cites W2050309905 @default.
• W2012509197 cites W2051525555 @default.
• W2012509197 cites W2053895186 @default.
• W2012509197 cites W2054538512 @default.
• W2012509197 cites W2057323262 @default.
• W2012509197 cites W2057368714 @default.
• W2012509197 cites W2059441082 @default.
• W2012509197 cites W2064649658 @default.
• W2012509197 cites W2075845648 @default.
• W2012509197 cites W2077675146 @default.
• W2012509197 cites W2078963630 @default.
• W2012509197 cites W2079244754 @default.
• W2012509197 cites W2080465107 @default.
• W2012509197 cites W2084777440 @default.
• W2012509197 cites W2087119984 @default.
• W2012509197 cites W2089425749 @default.
• W2012509197 cites W2090365812 @default.
• W2012509197 cites W2093433737 @default.
• W2012509197 cites W2109996424 @default.
• W2012509197 cites W2144677711 @default.
• W2012509197 cites W2150269343 @default.
• W2012509197 cites W2158652213 @default.
• W2012509197 cites W2170270268 @default.
• W2012509197 cites W2170632439 @default.
• W2012509197 cites W2315628981 @default.
• W2012509197 cites W2323904474 @default.
• W2012509197 cites W2588373281 @default.
• W2012509197 cites W4232059911 @default.
• W2012509197 cites W643643668 @default.
• W2012509197 doi "https://doi.org/10.1111/j.1365-2117.2011.00518.x" @default.
• W2012509197 hasPublicationYear "2011" @default.
• W2012509197 type Work @default.
• W2012509197 sameAs 2012509197 @default.
• W2012509197 citedByCount "18" @default.
• W2012509197 countsByYear W20125091972012 @default.
• W2012509197 countsByYear W20125091972015 @default.
• W2012509197 countsByYear W20125091972016 @default.
• W2012509197 countsByYear W20125091972017 @default.
• W2012509197 countsByYear W20125091972018 @default.
• W2012509197 countsByYear W20125091972019 @default.
• W2012509197 countsByYear W20125091972020 @default.
• W2012509197 countsByYear W20125091972021 @default.
• W2012509197 countsByYear W20125091972022 @default.
• W2012509197 countsByYear W20125091972023 @default.
• W2012509197 crossrefType "journal-article" @default.
• W2012509197 hasAuthorship W2012509197A5003572460 @default.
• W2012509197 hasAuthorship W2012509197A5004788351 @default.
• W2012509197 hasAuthorship W2012509197A5012673624 @default.
• W2012509197 hasAuthorship W2012509197A5016576526 @default.
• W2012509197 hasAuthorship W2012509197A5041988337 @default.
• W2012509197 hasAuthorship W2012509197A5050252452 @default.
• W2012509197 hasAuthorship W2012509197A5076031922 @default.
• W2012509197 hasAuthorship W2012509197A5085648951 @default.
• W2012509197 hasConcept C101433766 @default.
• W2012509197 hasConcept C109007969 @default.
• W2012509197 hasConcept C114793014 @default.
• W2012509197 hasConcept C120806208 @default.
• W2012509197 hasConcept C126559015 @default.
• W2012509197 hasConcept C127313418 @default.
• W2012509197 hasConcept C138496976 @default.
• W2012509197 hasConcept C15744967 @default.
• W2012509197 hasConcept C17409809 @default.
• W2012509197 hasConcept C183222429 @default.

• next