June 2022
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2 Reads
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2 Citations
Journal of the geological society of Korea
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June 2022
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2 Reads
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2 Citations
Journal of the geological society of Korea
March 2022
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4 Reads
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2 Citations
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
September 2021
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
June 2021
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3 Reads
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3 Citations
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
March 2021
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1 Read
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1 Citation
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
December 2020
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
September 2020
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1 Read
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2 Citations
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
August 2020
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2 Reads
Korean Cartographic Association
August 2020
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6 Reads
Journal of the Association of Korean Geographers
March 2020
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4 Reads
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3 Citations
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... These erosion basins typically have mountainous perimeters and lower-lying central areas, formed through processes like differential weathering and erosion. Within these basins, alluvial fans often form due to the accumulation of weathered layers and the presence of small streams [24,25]. However, the thickness of sediment layers in these alluvial fans is This study evaluates the prediction performance of N-V S models suggested in South Korea through residual analyses, using datasets acquired from the Busan region. ...
March 2022
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... Consequently, the estimation of uplift rates relies on changes in elevation and the depositional age of the marine terrace. Furthermore, spatial differences in uplift rates can be discerned by examining marine terraces formed around the same time but with varying elevations (Cucci and Cinti, 1998;Park et al., 2017;Lee and Park, 2020). Similarly, temporal disparities in uplift rates can be inferred by analyzing a series of marine terraces of different ages. ...
March 2020
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... 아울러, 이 같은 접근 방 식은 지표변형과 같이 활성조구조(active tectonics)와 관련된 다양한 지형이 분포하는 지역(e.g. Keller, 1986;Gürbüz and Gürer, 2008;Pedrera et al., 2009;Gao et al., 2013;Khalifa et al., 2018;Gupta et al., 2022) Lee et al., 2019a;Lee et al., 2019b;Oh, 2019;Hong et al., 2021;Kim and Seong, 2021 (Hack, 1973;Kirby and Whipple, 2003), 산지선단을 가로질러 흐르는 하천의 형태적 특 성은 지반융기에 의한 기준면의 고도변화를 반영한다 -86 -한국지형학회지 제29권 제4호(2022) (Wells et al., 1988). 따라서 지형지표는 지형발달 수준 (발달사적 혹은 지형진화적 측면)을 정량적으로 평가 하는 데 사용되거나, 지역 간 IRAT 분석에도 사용된다 (El Hamdouni et al., 2008). ...
March 2019
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... Studies on river terraces have predominantly focused on the eastern mountainous regions, i.e., the Taebaeksan and Sobaeksan mountain ranges, to determine the degree of ground uplift (Kim and Shin, 2014;Lee, 2018;Park, 2020a, 2021). Similarly, research on coastal terraces has concentrated on the eastern coast, where ground uplift has been active, with minimal studies conducted on the western and southern coasts (Choi et al., 2008;Choi, 2016;Park et al., 2017Park et al., , 2018aPark, 2019, 2020b;Shin et al., 2022a). ...
December 2018
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... First, the definition of the main fault remains uncertain and controversial. Several studies conducted during the 1970s termed the main structural feature aligned with the NNW-SSE-striking incised valley the "Ulsan Fault" (e.g., Kim, 1973;Kim et al., 1976;Kang, 1979a and b), but several subsequent studies adopted the term "Ulsan Fault Zone" to describe the various mapped and inferred NNW-SSE-to N-S-striking fault strands in and around the incised valley (e.g., Ryoo et al., 2000Ryoo et al., , 2001Ryoo et al., , 2002Ryoo et al., , 2004Ryoo, 2009;Lee et al., 2018). However, Okada et al. (1998) used the term "Ulsan Fault System" to describe NNW-SSE-striking neotectonic reverse faults that were mapped along the western front of the mountain range. ...
September 2018
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION
... Consequently, the estimation of uplift rates relies on changes in elevation and the depositional age of the marine terrace. Furthermore, spatial differences in uplift rates can be discerned by examining marine terraces formed around the same time but with varying elevations (Cucci and Cinti, 1998;Park et al., 2017;Lee and Park, 2020). Similarly, temporal disparities in uplift rates can be inferred by analyzing a series of marine terraces of different ages. ...
December 2017
JOURNAL OF THE KOREAN GEOMORPHOLOGICAL ASSOCIATION