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Paleomagnetic evidence for local oroclinal bending in the eastern Korean Peninsula
A paleomagnetic investigation has been carried out for the Lower Triassic Donggo Formation exposed in the Danyang area on the Yeongnam Massif to...
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A review of vertebrate body fossils from the Korean Peninsula and perspectives
For the first time, a comprehensive review was presented for all Korean vertebrate body fossils reported during last 100 years. At present, Korean...
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Introduction
The Korean Peninsula extends southward from the eastern end of the Asian continent. It is roughly 1000 km (621 miles) long and 216 km (134 miles)...
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Tectonic evolution of Precambrian basement massifs and an adjoining fold-and-thrust belt (Gyeonggi Marginal Belt), Korea: An overview
This contribution provides an overview on geology, geochronology, and tectonics of Precambrian basement massifs and adjoining Gyeonggi Marginal Belt...
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Early labechiid stromatoporoids of the Yeongheung Formation (Middle Ordovician), Yeongwol Group, mideastern Korean Peninsula: Part II. Systematic paleontology and paleogeographic implications
Three species belonging to two genera of labechiid stromatoporoids are described from the Yeongheung Formation (Darriwilian, Middle Ordovician),...
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Early labechiid stromatoporoids of the Yeongheung Formation (Middle Ordovician), Yeongwol Group, mideastern Korean Peninsula: Part I. Environmental distribution
This study examines depositional facies and environmental significance of early labechiid stromatoporoids in the Yeongheung Formation (late Middle...
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The 12 September 2016 Gyeongju earthquakes: 1. Observation and remaining questions
Two earthquakes ( M L 5.1 and 5.8) ruptured branches of the Yangsan Fault System in Gyeongju, S. Korea on September 12, 2016. After the M ...
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Spectral-induced polarization characterization of rocks from the Handuk iron mine, South Korea
Spectral-induced polarization (SIP) using the electrochemical reaction at the interface between mineral particle and groundwater is a powerful tool...
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Renewed profile of the Mesozoic magmatism in Korean Peninsula: Regional correlation and broader implication for cratonic destruction in the North China Craton
Widespread Mesozoic magmatism occurs in the Korean Peninsula (KP). The status quo is poles apart between the northern and southern parts in...
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Skarn zonation and rock physical properties of the Wondong Fe-Pb-Zn polymetallic deposit, Korea
The Wondong Fe-Pb-Zn polymetallic skarn deposit is located in the Taebaeksan Basin, South Korea. This deposit is associated with the Paleocene quartz...
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Revision of the conodont zonation of the uppermost Hwajeol Formation (Furongian), Taebaeksan Basin, Korea
The uppermost interval of the Hwajeol Formation, Taebaeksan Basin, has been assigned to the Fryxellodontus inornatus-Monocostodus...
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Forecasting and validation of landslide susceptibility using an integration of frequency ratio and neuro-fuzzy models: a case study of Seorak mountain area in Korea
Landslides susceptibility maps were constructed in Seorak mountain area, Korea, using an integration of frequency ratio and adaptive neuro-fuzzy...
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Depositional systems of the Lower Ordovician Mungok Formation in Yeongwol, Korea: implications for the carbonate ramp facies development
Detailed study on the Lower Ordovician Mungok Formation in the mideastern part of the Korean peninsula has led to recognition of seven lithofacies...
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First report of Cystostroma (Stromatoporoidea; Ordovician) from Sino-Korean Craton
A primitive stromatoporoid Cystostroma is reported from the Middle Ordovician Duwibong Formation of Taebaeksan Basin for the first time in Korea,...
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A case study for the integration of predictive mineral potential maps
This study aims to elaborate on the mineral potential maps using various models and verify the accuracy for the epithermal gold (Au) — silver (Ag)...
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Paleomagnetic results of the Late Permian Gobangsan Formation, Korean Peninsula: Remagnetization in the southeastern periphery of the Bagjisan Syncline
Sedimentary rocks in the Late Permian Gobangsan Formation were collected at 7 sites for paleomagnetic study in the southeastern periphery of the...
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Yellow Sea Transform Fault (YSTF) and the developemnt of Korean Peninsula
The Yellow Sea Transform Fault ( YSTF ), the boundary between the Korean Peninsula and the South China Plate was a repeatedly reactivated ancient...
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The Okcheon Supergroup in the Lake Chungju area, Korea: Neoproterozoic volcanic and glaciogenic sedimentary successions in a rift basin
The Okcheon Belt in southern Korea is an NE-SW trending fold-and-thrust belt consisting of two sedimentary basins of different origins: namely, the...
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Early Ordovician reefs from the Taebaek Group, Korea: constituents, types, and geological implications
The Early Ordovician (early to middle Floian) bioherms of the Dumugol Formation, Korea, are compiled and their paleoenvironmental and paleogeographic...
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Middle Furongian (late Cambrian) polymerid trilobites from the upper part of the Sesong Formation, Taebaeksan Basin, Korea
The upper part of the Sesong Formation of the Taebaek Group, Taebaeksan Basin, Korea, is known to contain the Kaolishania Zone which can be equated...