FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4285294071> ?p ?o ?g. }

• W4285294071 abstract "Abstract In this review, we attempted to summarize and interpret the Phanerozoic geology and mineralization following the article (vol. 71 in Resource Geology) which reviewed the Precambrian geology and mineralization of North Korea. The basement of the Korean peninsula was built during the Precambrian and gradually became more evolved and complex during the Phanerozoic. The northern part of the peninsula was in the active and passive continental margins of the Korea–China platform during the Phanerozoic. In the tectonic environments of the Phanerozoic, the tectonic provinces of North Korea comprise several Paleozoic–Mesozoic intracontinental and rift basins as well as Cenozoic ocean border and rift basins. During the Paleozoic, the sedimentary strata were formed within the marine‐to‐nonmarine intracontinental basins, such as the largest Pyeongnam and Hyesan–Iwon basin, Imjingang rift basin, and several small structural basins, and the sedimentary type of limestone, dolomite, and coal deposits were formed. Mesozoic orogenic events in the peninsula were the most overwhelming geologic event causing block movements through collision and subduction of the paleo‐Pacific plate. Songrim orogeny (late Permian to early Triassic) might be caused by continental collision associated with strong deformation, metamorphism, and granite intrusion. Daebo orogeny (Jurassic) resumed the crustal deformation under a contractional setting during the subduction and caused dextral ductile shearing, magmatism, and metamorphism in the entire peninsula. Amnokgang orogeny, corresponding to Bulguksa orogeny in South Korea, during the Cretaceous formed several pull‐apart or transtensional basins probably because of oblique subduction of the Izanagi plate, and nonmarine sedimentary and pyroclastic sequences were deposited in the basin. The mineralization related to the Mesozoic plutonism was the most dominant in the peninsula. The considerable mineral deposits are ultramafic related magmatic Ni deposits owing to rift magmatism and granite related hydrothermal Au–Ag, Cu, Pb–Zn, Fe, W, and Mo deposits caused by the subduction of paleo‐Pacific plate. During the Tertiary, several structural basins under the extensional regime were overprinted on the Mesozoic basins in the northern part of the peninsula. They contain marine and nonmarine sedimentary rocks and felsic–mafic extrusives. Some sedimentary deposits, such as coal, kaolin, bentonite, diatomite, and zeolite, were formed. The Tertiary Pohang basin in South Korea shows basin geology, magmatism, and mineralization similar to those of North Korea. The Phanerozoic geotectonics of the peninsula are characterized by the evolution of the structural basins and violent magmatism. The peninsula is located on the Amur plate, bounded by the Philippine plate, Pacific plate, and Eurasian plate. Since Phanerozoic, the peninsula's geographic position created an important tectonic link between northeastern China and the Japanese Islands throughout geotectonic evolution." @default.
• W4285294071 created "2022-07-14" @default.
• W4285294071 creator A5001386598 @default.
• W4285294071 creator A5013116405 @default.
• W4285294071 creator A5038018230 @default.
• W4285294071 creator A5054722078 @default.
• W4285294071 creator A5089257266 @default.
• W4285294071 date "2022-01-01" @default.
• W4285294071 modified "2023-10-18" @default.
• W4285294071 title "Review on geology and mineralization of <scp>North Korea</scp> ( <scp>II</scp> : <scp>Phanerozoic</scp> )" @default.
• W4285294071 cites W2000795509 @default.
• W4285294071 cites W2011159906 @default.
• W4285294071 cites W2025226620 @default.
• W4285294071 cites W2063648931 @default.
• W4285294071 cites W2084183702 @default.
• W4285294071 cites W2169534787 @default.
• W4285294071 cites W3196348347 @default.
• W4285294071 cites W3200646995 @default.
• W4285294071 doi "https://doi.org/10.1111/rge.12293" @default.
• W4285294071 hasPublicationYear "2022" @default.
• W4285294071 type Work @default.
• W4285294071 citedByCount "1" @default.
• W4285294071 countsByYear W42852940712022 @default.
• W4285294071 crossrefType "journal-article" @default.
• W4285294071 hasAuthorship W4285294071A5001386598 @default.
• W4285294071 hasAuthorship W4285294071A5013116405 @default.
• W4285294071 hasAuthorship W4285294071A5038018230 @default.
• W4285294071 hasAuthorship W4285294071A5054722078 @default.
• W4285294071 hasAuthorship W4285294071A5089257266 @default.
• W4285294071 hasBestOaLocation W42852940711 @default.
• W4285294071 hasConcept C109007969 @default.
• W4285294071 hasConcept C127313418 @default.
• W4285294071 hasConcept C13106087 @default.
• W4285294071 hasConcept C151730666 @default.
• W4285294071 hasConcept C167570900 @default.
• W4285294071 hasConcept C173776410 @default.
• W4285294071 hasConcept C17409809 @default.
• W4285294071 hasConcept C200646496 @default.
• W4285294071 hasConcept C2777241186 @default.
• W4285294071 hasConcept C50682988 @default.
• W4285294071 hasConcept C58097730 @default.
• W4285294071 hasConcept C6494504 @default.
• W4285294071 hasConcept C73707237 @default.
• W4285294071 hasConcept C77928131 @default.
• W4285294071 hasConcept C93033518 @default.
• W4285294071 hasConceptScore W4285294071C109007969 @default.
• W4285294071 hasConceptScore W4285294071C127313418 @default.
• W4285294071 hasConceptScore W4285294071C13106087 @default.
• W4285294071 hasConceptScore W4285294071C151730666 @default.
• W4285294071 hasConceptScore W4285294071C167570900 @default.
• W4285294071 hasConceptScore W4285294071C173776410 @default.
• W4285294071 hasConceptScore W4285294071C17409809 @default.
• W4285294071 hasConceptScore W4285294071C200646496 @default.
• W4285294071 hasConceptScore W4285294071C2777241186 @default.
• W4285294071 hasConceptScore W4285294071C50682988 @default.
• W4285294071 hasConceptScore W4285294071C58097730 @default.
• W4285294071 hasConceptScore W4285294071C6494504 @default.
• W4285294071 hasConceptScore W4285294071C73707237 @default.
• W4285294071 hasConceptScore W4285294071C77928131 @default.
• W4285294071 hasConceptScore W4285294071C93033518 @default.
• W4285294071 hasFunder F4320322097 @default.
• W4285294071 hasFunder F4320325370 @default.
• W4285294071 hasIssue "1" @default.
• W4285294071 hasLocation W42852940711 @default.
• W4285294071 hasOpenAccess W4285294071 @default.
• W4285294071 hasPrimaryLocation W42852940711 @default.
• W4285294071 hasRelatedWork W1678053888 @default.
• W4285294071 hasRelatedWork W1963584426 @default.
• W4285294071 hasRelatedWork W2001949408 @default.
• W4285294071 hasRelatedWork W2022575623 @default.
• W4285294071 hasRelatedWork W2032082002 @default.
• W4285294071 hasRelatedWork W2042106659 @default.
• W4285294071 hasRelatedWork W2081753728 @default.
• W4285294071 hasRelatedWork W2419529650 @default.
• W4285294071 hasRelatedWork W2546506658 @default.
• W4285294071 hasRelatedWork W4237866904 @default.
• W4285294071 hasVolume "72" @default.
• W4285294071 isParatext "false" @default.
• W4285294071 isRetracted "false" @default.
• W4285294071 workType "article" @default.