ScholarWorks@Gyeongsang National University: Sohn, Young Kwan

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Sohn, Young Kwan (손영관)

자연과학대학 (지질과학과)

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Tel 0557721476
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Jeju Island:24||Gyeongsang Basin:9||제주도:7||Eoil Basin:6||Sudan:6||Tuff ring:5||Korea:5||ignimbrite:5||tuff ring:5||Dadaepo Basin:4||Diatreme:4||Pohang Basin:4||Holocene:4||hydrovolcanism:4||Hydrovolcanism:3||stable isotope:3||Seoguipo Formation:3||pullapart basin:3||Surtseyan eruption:3||pyroclastic density current:3||Janggi Basin:3||Zircon:3||volcaniclastics:3||Kusandong Tuff:3||Tuff cone:3||Seamount:3||alteration:3||Pullapart basin:3||Middle Stone Age:3||Fan delta:3||어일분지:3||lithic technology:3||Young Kwan Sohn:3||경상분지:3||Acheulean:3||phreatomagmatism:3||구산동응회암:3||수성화산활동:3||lava flow:3||stratigraphy:2||이원성 화산활동:2||자기미세구조:2||stromatolite:2||Alkali basalt:2||장기분지:2||correlation:2||Island(ChangSik Cheong and YounJoong Jeong:2||syntectonic volcanism:2||Dadaepo Formation:2||Daejeon 305333:2||diatreme:2||Phreatomagmatic eruption:2||지질유산:2||Phreatomagmatism:2||Maar:2||층서:2||eruptive unit:2||Pleistocene:2||tuff cone:2||Tephra:2||flow transformation:2||Ignimbrite:2||Debris flow:2||Propagating rifting:2||East Sea:2||volcanism:2||Basalt geochemistry:2||hyaloclastite:2||Intraplate volcanism:2||UTh age:2||화산쇄설암:2||East Sea opening:2||화쇄류암:2||Caldera:2||전기 마이오세:2||Ulleung Island:2||lithification:2||Vent migration:2||maar:2||Department of Earth and Environmental Sciences:2||당겨열림분지:2||Millennium Eruption:2||Volcaniclastic sedimentation:2||대자율이방성:2||modal composition:2||Waup Basin:2||Goseong Formation:2||Yeonil Tectonic Line:2||Cretaceous:2||방사성탄소연대:2||Jinju 660701:2||paleoclimate:2||Baekdusan:2||absolute age:2||Korea Basic Science Institute:2||OSL:2||Gusandong Tuff:2||Gyeongsang National University:2||Hakbong Basalt:2||연대측정:2||basaltic glass:2||Hamori Formation:2||basin evolution:2||bimodal volcanism:2||scoria cone:2||용암류:2||Sinyangdong Formation:2||chemical composition:2||Hanon crater:2||smectite:2||Hayang Group:2||Cheongryongsa Basalt:2||Division of Isotope Geoscience:2||Middle Pleistocene:1||Miocene stratigraphy:1||Miryang block:1||Monogenetic:1||Monogenetic eruptions:1||Monogenetic volcanism:1||Mt. Hallasan:1||Noeseongsan Basaltic rock:1||O isotope:1||OHf isotopes:1||OSL dating:1||Oceanic volcanic island:1||Ocheon Fault System:1||Optically stimulated luminescence:1||Optically stimulated luminescence (OSL) dating:1||Pacific plate:1||Palaeoenvironment:1||Paleoheating temperature estimation:1||Paleocurrent:1||Paleomagnetic analysis:1||Paleomagnetism:1||Paleomagnetism and rock (sediment) magnetism:1||Paljori Tuff:1||Peperite:1||Petrography:1||Phreatomagmatic Volcano:1||Plate tectonics:1||Pleistocene fluvial deposits:1||Plumbing system:1||Pohang basin:1||ProtoPacific (Izanagi/Kula) plate:1||Pseudotachylyte:1||Pyroclastic:1||Pyroclastic current:1||Pyroclastic density current:1||Pyroclastic surge:1||Quaternary:1||Radiocarbon age:1||Rare earth elements:1||Recycled ancient silicate sediment:1||Recycled diatoms:1||Rejuvenation:1||Rhodoid:1||Rock (sediment) magnetism:1||Rock cleavage:1||Ross Sea:1||SEM:1||Scaling analysis:1||Sea Cave:1||Sea of Japan:1||Sedimentary facies:1||Seongdongri Formation:1||Seongsan Ilchulbong:1||Seongsan Ilchulbong Tuff Cone:1||Sequence stratigraphy:1||Sequence stratigrphy:1||Sinistral pullapart basin:1||Site formation processes:1||SrNdPbHfMg isotopes:1||Stratigraphic development:1||Stratigraphy:1||Subaqueous dune:1||Submarine channel:1||Submarine volcanism:1||Surtseyan volcanism:1||Syneruption:1||Synrift:1||Syntectonic deposition:1||Syntectonic volcanism:1||Synvolcanic tectonism:1||TEM:1||Taalian eruption:1||Tephra componentry:1||Th230/U234 ages:1||Tianchi excursion:1||Trachyte:1||Transfer zone:1||Tuffisite:1||Tuffring:1||UPb age:1||Udo Island:1||Uiseong block:1||Ulleung:1||Ulleung Basin:1||Vesiculated tuff:1||Volcanic geoheritage:1||Volcaniclastic:1||Volcaniclastic apron:1||Volcano morphology:1||Volcanogenic sedimentation:1||Yangpo subbasin:1||Yangsan fault system:1||YounJoong Jeong:1||Zeolite:1||aa:1||active layer:1||age dating:1||analcime:1||anisotropy of magnetic susceptibility:1||antarctic continental margin:1||arc volcanism:1||backarc:1||backarc basin:1||backarc basin:1||basalt geochemistry:1||basin configuration:1||carbonate concretion:1||chemistry:1||clastic dikes:1||clinoptilolite:1||clockwise rotation:1||composite tuff cone:1||continental arc:1||continental rifting:1||debris flow:1||depositional environment:1||depositional process:1||depositional processes:1||dextral simple shear:1||earthquakeinduced liquefaction:1||effusive eruptions:1||emplacement mechanism:1||explosive eruptions:1||flood:1||flow indicator:1||fluvial deposit:1||fluvial sediments:1||footprint:1||geoheritage:1||geomonitoring:1||glaciomarine laminated muds:1||glass:1||glass shard:1||half graben:1||hyperconcentrated flow:1||intraarc basin:1||intraplate volcanism:1||inverse magnetic fabric:1||jeju island:1||lahar:1||lake margin:1||luminescence dating:1||magma plumbing system:1||magnetic fabric:1||mantle upwelling:1||mineralogy:1||miocene:1||mollusk shells:1||monogenetic volcano:1||mordenite:1||mountain stream:1||natural heritage:1||no:1||normal magnetic fabric:1||pāhoehoe lava:1||pahoehoe:1||paleoceanography:1||paleomagnetism:1||paleosol:1||patterned ground:1||periglacial landform:1||permafrost:1||phillipsite:1||phonolite:1||pullapart:1||pyroclastic surge:1||quartz:1||quartz OSL dating:1||quaternary volcanism:1||radiocarbon age:1||radiocarbon dating:1||resedimentation:1||saline aquifer:1||scissor fault:1||sedimentary environment:1||shield volcano:1||site formation process:1||songaksan tuff:1||source evolution:1||stratigraphic development:1||stratigraphic trap:1||stratigraphy1. INTRODUCTIONThe Gyeongsang Basin is the largest Cretaceous basin inKorea:1||strontium isotope:1||submarine channel:1||submarine volcanic exploration:1||suwolbong tuff:1||tectonic inversion:1||tectonics:1||tephra:1||tephra componentry:1||texture:1||thermal enhancement:1||thermobarometry:1||trachyte:1||tuff:1||underground CO2 storage:1||usewear:1||vent migration:1||vesicle number density:1||vesicularity:1||volcanic neck:1||volcaniclastic deposit:1||volcaniclastic sediment:1||wave cut:1||wave erosion:1||wave planation:1||which developed on an arc masif in the easternmargin of the Eurasian continent associated with the subduction of a:1||zeolitization:1||‘a‘ā lava:1||거문오름용암동굴계:1||거창:1||결:1||고기후:1||고성층:1||고자기:1||고토양:1||고화작용:1||곶자왈:1||구조동시성 화산활동:1||구조토:1||남극:1||뇌성산현무암질암:1||다대포분지:1||다대포층:1||다이아트림:1||대비:1||대염수층:1||데사이트질 화산활동:1||동해 확장:1||라하:1||마르:1||마이오세 층서:1||모드조성:1||밀양지괴:1||발자국:1||백악기:1||변질작용:1||분석구:1||분지지형:1||분출단위:1||불석:1||섯치형 분출:1||섯치형 분화:1||성동리층:1||성산일출봉:1||성산일출봉 응회구:1||수성화산체:1||스멕타이트:1||스트로마톨라이트:1||신양동층:1||아날심:1||아아:1||안정동위원소:1||양포소분지:1||역미세구조:1||연일구조선:1||열이온화질량분석법:1||영구동토:1||와읍분지:1||용암동굴:1||우도:1||우라늄계열 비평형:1||우수향 단순전단:1||유리 샤아드:1||유변환:1||응력반전:1||응회구 복합체:1||응회환:1||의성지괴:1||이산화탄소 지중저장:1||입천소분지:1||자기미세구조의 열적 향상:1||자연유산:1||장기역암:1||전촌응회구:1||전파열개:1||절대연대:1||정미세구조:1||제4기 화산암:1||제주도ChangSik Cheong:1||주빙하지형:1||지질모니터링:1||지질지표:1||청룡사현무암:1||층서 트랩:1||킹조지섬:1||타알형 분출:1||테프라:1||퇴적환경:1||파호이호이:1||팔조리응회암:1||포항분지:1||필립사이트:1||하논 분화구:1||하모리층:1||하양층군:1||학봉현무암:1||한라산:1||해빈퇴적물:1||해식동굴:1||해저 화산탐사:1||현무암질 유리:1||홀로세:1||홍조단괴:1||화강암 석재:1||화도이동:1||화산쇄설성 밀도류:1||화산쇄설성 퇴적물:1||화산활동:1||화학조성:1||1722 ka period:1||활동층:1||2006:1||AMS:1||AMS (anisotropy of magnetic susceptibility):1||Accretionary lapilli:1||Acheulean artifacts:1||Aeolian dune:1||Alluvial fan:1||Anisotropy of magnetic susceptibility (AMS):1||Antarctic continental margin:1||Antarctica:1||Ar40/Ar39 dating:1||Architectural element:1||Architectural elements:1||Ash aggregation:1||Backarc:1||Baekdusan (Changbaishan):1||Baked sediment:1||Bangudae Petroglyphs:1||Basalt:1||Basin evolution:1||Beach Sediments:1||Biogenic components:1||Blockandash flow:1||Caldera fault zone:1||Carbonated eclogite:1||Climateproductivity model:1||Clinker:1||Coarsegrained delta:1||Continental shelf:1||Crustal cannibalization:1||Cryptodome explosion:1||Dacitic volcanism:1||Deepsea channel system:1||Deepsea conglomerate:1||Depositional process:1||Depositional processes:1||Dextral shear:1||Dimensionless parameter:1||Dokdo:1||Dunefield pattern:1||EDAR:1||Early Eocene:1||Early Miocene:1||East Sea (Sea of Japan):1||Eastern desert:1||Eruptive episode:1||Facies architecture:1||Fault intrusions:1||Flood basalt:1||Fluvial:1||Fluvial environment:1||Fluvial topography:1||Footprint:1||Foredeep:1||Frictional melting:1||Gampo Conglomerate:1||Geochang:1||Geochemistry:1||Geoheritage:1||Geoindicatir:1||Geologic age:1||Geomagnetic instability:1||Geomunoreum Lava Tube System:1||Global sealevel cycle:1||Gosan formation:1||Gotjawal:1||Granite stone:1||Hantangang River Volcanic Field:1||Hf isotopes:1||Hilina Pali excursion:1||Holocene sealevel change:1||Hominid:1||Hominin dispersal:1||Hydrovolcanic sequence:1||Ilchulbong tuff cone:1||Intereruption:1||Intraplate volcanic fields:1||Introduction to sample preparation and thermal ionization mas spectrometry for 238U230Th dating of Korea. v. 42:1||Ipcheon Subbasin:1||Iran:1||Isotopes:1||Janggi Conglomerate:1||Jeju:1||Jeju island:1||Jeonchon tuff cone:1||King George Island:1||Kusandong Tuf:1||Lacustrine:1||Lago Sofia Conglomerate:1||Lapilli tuff:1||Large Cutting Tools:1||Late PleistoceneHolocene volcanism:1||Lava Tube Cave:1||Lava flow:1||Lavasediment interaction:1||Lithofacies:1||Lowaspectratio ignimbrite:1||Luminescence dating (OSL):1||MC ICPMS:1||MIS 5:1||MSA:1||Maardiatreme volcano:1||Magmawater interaction:1||Magnetic fabric:1||Magnetic minerals:1||Magnetic susceptibility:1||Magnetics fabric:1||Man Sik Choi and ByongKwon Park:1||Mantle plumes:1||Mantle source melting:1||Mantle transition zone:1||Material property:1||

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