ScholarWorks@Korea University: SEONG, Yeong Bae

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SEONG, Yeong Bae (성영배)

College of Education (Department of Geography Education)

Research Area: 지형, 기후변화, 제4기, Geomorphology, Climate Change, Quaternary

Tel 02-3290-2367
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OSL dating:6||Antarctica:6||Quaternary:5||Holocene:4||active fault:4||Deglaciation:4||Cosmogenic nuclides:3||DEM:3||sea level change:3||Baekdusan:2||Spillover:2||Be10 surface exposure dating:2||Quaternary fault:2||Catchmentwide denudation rate (CWDR):2||빙하:2||erosion:2||Mongolian Altai:2||Geomorphology:2||우주선유발 동위원소:2||백두산:2||10Be:2||cosmogenic Be10:2||Climate change:2||Catchmentwide denudation rate:2||strikeslip fault:2||무등산:2||Pleistocene:2||landscape evolution:2||Geomorphic equilibrium:2||Be10 exposure dating:2||TabunKhara:2||OSL 연대측정:2||활성단층:2||cosmogenic nuclides:2||Glacier:2||Aggradation:1||Lake overflow:1||CheolwonPyeongang Lava Plateau:1||Glacial geomorphology:1||Larsen ice shelf:1||Episodic erosional processes:1||transverse drainage:1||Process domains:1||Uplift rate:1||Daegwanryeong Plateau:1||관모봉:1||토양유실:1||분리제어환경:1||유역분지형태:1||미세구조:1||periglacial climate:1||Scaledependency:1||주빙하성 평활사면:1||Mt. Moodeung:1||tectonic uplift:1||구조토:1||Detrital zircon:1||grazing:1||운석충돌구:1||Be isotope:1||raised beach:1||sea level:1||Indian summer monsoon rainfall:1||recent earthquake:1||lockin depth:1||sliprate:1||divide migration:1||Peninsular India:1||Coastal cliff:1||Cosmogenic nuclides surface exposure dating:1||Alluvial fan:1||Pediment:1||Bouldery deposit:1||active faults map:1||paleoseismology:1||Divide migration:1||Gilbert metrics:1||철원평강 용암대지:1||Chugaryeong Tectonic Valley:1||OSL age dating:1||paleofluvial deposits:1||paleolacustrine deposits:1||Periglacial:1||Paleoclimate:1||Beryllium10 (Be10):1||Disturbance:1||Ephemeral channel:1||desert geomorphology:1||peneplain:1||Stream longitudinal profile:1||Sink:1||Flow routing:1||Morphological Descriptors Analysis:1||인류세:1||MIS 7:1||Siberian high pressure (SHP):1||Midlatitude westerlies:1||Loess:1||fixed window smoothing:1||interpolation at each contour interval:1||평활화:1||침식관련 계수 K:1||1dimension numerical model:1||micromorphology:1||striation:1||nivation:1||Active tectonics:1||displacement:1||동결작용:1||central Karakoram:1||Himalaya:1||Mountain growth:1||Fold growth:1||rocky shore:1||coastal retreat:1||Cosmogenic burial dating:1||광여기루미네선스:1||Be10 denudation rates:1||soil erosion:1||UAV (Unmanned Aerial Vehicle):1||cliff retreat:1||cosmogenic(36)Cl:1||East coast of India:1||magnetic stratigraphy:1||Yangsan fault:1||the Quaternary fault:1||변위율:1||지진규모:1||topographic parameter:1||Holocene shoreline:1||대자율:1||Magnetic susceptibility:1||Western Mongolia:1||Cliff erosion:1||Rock coasts:1||Shore platform:1||항공사진:1||lineament:1||Geochronology:1||Local Last Glacial Maximum:1||Mt. Melbourne Volcano:1||Colorado River:1||Landslide:1||전곡 용암대지:1||Jeongok Lava Plateau:1||cosmogenic surface dating:1||ice sheet:1||10Be 수직단면 연대측정:1||Yugye Fault:1||Cosmogenic isotopes:1||Insitu C14:1||Rockwall retreat:1||piracy:1||Cirque:1||형태요소분석:1||soil production function:1||토양생성률:1||Cosmogenic10Be surface exposure dating:1||Optically stimulated luminescence (OSL) dating:1||일정 고도 간격 이동창 평활화:1||기반암 하상:1||암석해안:1||파식대:1||범람원:1||우주선:1||Mt. Mudeung:1||Landform classification:1||표면노출연대:1||cosmogenic Be10 dating:1||incision rate:1||Blind thrust:1||Lateral fold propagation:1||Altyn Tagh Fault:1||sorting:1||glaciation:1||geochronology:1||Queen Creek:1||울산단층:1||제4기단층:1||faulting age:1||무인동력비행장치:1||surface geometry:1||Ross Sea:1||subhorizontal platform:1||sea ice:1||local contamination offset:1||East Antarctic Ice Sheet:1||Last Glacial Maximum:1||Glacier reconstruction:1||LiDAR:1||제4기 단층:1||catchmentwide denudation rate:1||삼각주:1||입도 분석:1||zoogeomorphology:1||glacial lakes:1||morphometric analysis:1||Sea level rise:1||Lava dammed lake:1||Lacustrine terrace:1||Glaciovolcanic Process:1||Base level:1||Colorado Plateau:1||Little Colorado River:1||Cosmogenic exposure dating:1||Outburst flood deposit:1||Fluvial terrace:1||Monte Carlo Simulation:1||지형지시자:1||Glaciation:1||superimposition:1||base level:1||surface reconstruction:1||soil production rate:1||Central Asia:1||streamwise increasing window smoothing:1||cosmogenic nuclides(CNs):1||burial dating:1||rock coast:1||OSL 연대:1||reddish band:1||clay mineral:1||Cliff retreat:1||inheritance:1||주빙하기후:1||cosmic ray:1||지형패턴:1||지형분류:1||무감독분류:1||glacier:1||slip rate:1||climate forcing:1||Foreberg:1||Endoreic:1||Midbruhnes event:1||지표기하:1||Environmental magnetism:1||Chilika Lagoon:1||Core monsoon zone:1||선형구조:1||Tien Shan:1||Overfill:1||Transverse stream:1||Drainage integration:1||Terra Nova bay:1||Kherlen fault:1||quaternary geomorphology:1||추가령 구조곡:1||고하성층:1||우주선유발 방사성동위원소:1||유계단층:1||Meteoric Be10:1||Debris flow:1||weathering:1||catchmentwide denudation:1||anthropocene:1||등고선 간격별 내삽 평활화:1||smoothing:1||depth profile dating:1||shore platform:1||floodplain:1||wavecut platform:1||동경포행:1||solifluction:1||freezing and creeping:1||Geomorphons:1||Unsupervised classification:1||cosmogenic 36Cl surface exposure age:1||찰흔:1||stream piracy:1||Tibet:1||monsoon:1||Victoria land:1||land use changes:1||differential uplift:1||remanence recording efficiency:1||양산단층:1||surface rupture:1||Lava flow:1||단층지형:1||Proglacial lakes:1||Tectonic scarps:1||Paleo earthquake:1||Piracy:1||Inexpressible island:1||Extensional basin margin:1||OSL 연대 측정:1||고호소층:1||Marguerite Bay:1||Morainedammed lake:1||Cosmogenic 10Be:1||하안단구:1||몬테 카를로 시뮬레이션:1||천이점:1||Seti River:1||Knickzone:1||Korean Peninsula:1||확률분석:1||고정 이동창 평활화:1||하류 증대 이동창 평활화:1||1차원 수치 하천종단 발달 모형:1||융기율:1||Bedrock channel:1||매몰연대측정:1||sea cliff:1||암설지형:1||debris landform:1||설식:1||cryoplanation surface:1||fluvial strath terrace:1||knickpoint migration:1||Cosmogenic Be10 dating:1||cosmogenic 10Be dating:1||patterned ground:1||frost action:1||coastal erosion:1||cosmogenic nuclide:1||Salt River:1||단층활동연대:1||Ulsan fault:1||arid lands:1||지중기하:1||Cosmogenic nuclide exposure dating:1||topographic analysis:1||relative paleointensity:1||Indian Summer Monsoon:1||moment magnitude:1||tectonic geomorphology:1||Delta:1||기후 변화:1||Siberian High:1||Cosmogenic:1||lithology:1||faultrelated landform:1||aerial photo:1||Pohang earthquake:1||Ross ice shelf:1||Shoreline:1||Depth Profile Dating:1||geomorphic marker:1||knickpoint:1||주향이동단층:1||Block streams:1||Soils:1||paleosurface:1||Pit:1||권곡:1||Jeongdongjin coastal terrace:1||Uplift rates:1||fixed height interval based window smoothing:1||하천종단:1||stream profile:1||Detachmentlimited channel:1||단순노출연대측정:1||수직단면연대측정:1||해식애:1||점토 광물:1||솔리플럭션:1||surface exposure age:1||numerical model:1||Exoreic:1||land degradation:1||wildfire:1||subsurface geometry:1||oceanic sedimentation:1||Yangsan Fault:1||Paleodenudation:1||frost cracking:1||Fluvial geomorphology:1||인도 반도:1||하천지형:1||시베리아 고기압:1||Grain size analysis:1||geomorphological criteria:1||Khorgo:1||paleoseismological investigation:1||Glacial lake outburst flood (GLOF):1||Well Cuttings:1||Campbell glacier:1||Stream terrace:1||Overflow:1||Extensional tectonic terrain:1||Bidahochi Formation:1||Earthquake:1||age dating:1||palaeoclimate:1||Lake Khagiin Khar:1||antecedence:1||overflow:1||Landform evolution:1||Ecosystem:1||soil production:1||Depression:1||Gwanmo Massif:1||Probability Analysis:1||soil loss:1||토양생성함수:1||가속기질량분석기:1||AMS(Accelerator Mass Spectrometry) simple surface exposure dating:1||해수면 변동:1||적색 밴드:1||스케일종속성:1||우주선 유발 동위원소 36Cl 노출연대:1||Channel deflection:1||분급:1||토양요동현상:1||cryoturbation:1||mountain glaciation:1||Geomorhic metrics:1||Mineral logs:1||OSL:1||Ross sea:1||urban construction:1||natural background rate:1||impact crater:1||luminescence dating:1||western North Pacific:1||fault slip rates:1||thrust fault:1||홀로세 구정선:1||climate:1||sediment:1||LavaWaterInteraction feature:1||Sonoran Desert:1||IssykAta fault:1||Kyrgyz Range:1||

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