Neoproterozoic and middle Paleozoic geological events in the eastern Wolhyeonri complex of the southwestern Gyeonggi Massif, South Korea, and their tectonic correlations in northeastern Asia

Lithos ◽  
2021 ◽  
Vol 382-383 ◽  
pp. 105923
Author(s):  
Takeshi Imayama ◽  
Chang Whan Oh ◽  
Jimin Jeon ◽  
Keewook Yi
Tectonics ◽  
1991 ◽  
Vol 10 (6) ◽  
pp. 1130-1151 ◽  
Author(s):  
Dominique Cluzel ◽  
Laurent Jolivet ◽  
Jean-Paul Cadet

2015 ◽  
Vol 17 (1) ◽  
pp. 437-451 ◽  
Author(s):  
Jinyoung Rhee ◽  
Jaepil Cho

Abstract The future changes in drought characteristics were examined on a regional scale for South Korea, in northeastern Asia, using 17 bias-corrected projections from phase 5 of the Coupled Model Intercomparison Project (CMIP5) of representative concentration pathway (RCP) scenarios 4.5 and 8.5. The frequency of severe or extreme drought, based on the standardized precipitation index (SPI) and standardized precipitation evapotranspiration index (SPEI), with time scales of 1, 3, and 12 months (i.e., SPI1, SPI3, SPI12, SPEI1, SPEI3, and SPEI12), was considered, as well as the average duration based on SPEI1. A multimodel ensemble (MME) was produced using selected models, and future changes were investigated in terms of both drought frequency and the average duration for the entire area and four river basins. The changes in drought frequency largely depend on the selection of a drought index, rather than climate projection scenarios. SPEI3 mostly projected future increases in drought frequency, while SPI3 showed varied projections. SPI12 projected decreases in drought frequency for both scenarios in the study area, while differences between river basins were observed for SPEI12. Increases in the average duration of droughts were projected based on SPEI1, indicating an increase in persistent short-term droughts in the future. The results emphasize the importance of regional- and subregional-scale analysis in northeastern Asia. The findings of the study provide valuable information that can be used for drought-related decision-making, which could not be obtained from studies on a global spatial scale.


2014 ◽  
Vol 95 ◽  
pp. 203-216 ◽  
Author(s):  
Chang-Whan Oh ◽  
Takeshi Imayama ◽  
Sang-Bong Yi ◽  
Taeseong Kim ◽  
In-Chang Ryu ◽  
...  

2005 ◽  
Vol 142 (1) ◽  
pp. 23-30 ◽  
Author(s):  
MINGGUO ZHAI ◽  
ZHIYAO NI ◽  
CHANG WHAN OH ◽  
JINGHUI GUO ◽  
SEON GYU CHOI

A large rapakivi granite batholith in the Neo-Archaean/Palaeoproterozoic Odesan complex, northeastern Gyeonggi massif, South Korea, has been dated at 1839±10 Ma using SHRIMP U–Pb analysis of zircons. The age, petrological and geochemical characteristics of this batholith are similar to those of the rapakivi granite batholiths exposed in the Rangnim massif of North Korea and in the Miyun–Chengde complex of North China. The country rocks of these rapakivi granite batholiths are also comparable; all are composed of granitic gneisses and banded iron formation (BIF)-bearing supracrustal rocks metamorphosed to amphibolite- to granulite-facies. This study provides new evidence for the suggestion that the Gyeonggi and Rangnim massifs may share an affinity with the Precambrian basement of the North China craton. The study provides new insight into the possible eastward extension of the Sulu orogenic belt in the Korean peninsula and further provides evidence to correlate the Korea basement to a possible global 2.1–1.8 Ga supercontinent.


2008 ◽  
Vol 12 (1) ◽  
pp. 1-6 ◽  
Author(s):  
Moonsup Cho ◽  
Hyeoncheol Kim ◽  
Yuyoung Lee ◽  
Kenji Horie ◽  
Hiroshi Hidaka

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