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Imjingang Belt

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Journal Article
Journal: Geology
Published: 01 December 1996
Geology (1996) 24 (12): 1071–1074.
...Jin-Han Ree; Moonsup Cho; Sung-Tack Kwon; Eizo Nakamura Abstract Structural, petrological, and geochronological data from the middle Korean peninsula indicate that the Qinling-Dabie-Sulu collisional belt of east-central China crosses the Yellow Sea and extends into the Imjingang belt. The Yeoncheon...
Journal Article
Published: 01 April 2009
American Mineralogist (2009) 94 (4): 430–438.
...Yoonsup Kim; Keewook Yi; Moonsup Cho Abstract The paragenetic relationships and Th-U distributions among allanite, monazite, and xenotime were investigated in a progressive sequence of garnet- to kyanite-zone metapelites of the Imjingang belt, Korea. Allanite is predominant in the garnet...
FIGURES | View All (6)
Journal Article
Published: 01 September 2000
European Journal of Mineralogy (2000) 12 (5): 1057–1062.
...Jinho AHN; Moonsup CHO Abstract Cathodoluminescence (CL) was used to investigate the mode and compositional zoning of plagioclase in fine-grained metapelites of the Imjingang Belt, Korea. Minute, untwinned grains of plagioclase are indistinguishable from quartz under the polarized light microscope...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP280.14
EISBN: 9781862395282
..., belonging to the Sino-Korea, Yangtze and Cathaysia tectonic units. In the vicinity of Qingdao–Rizhao, the Wulian–Qingdao–Imjingang orogen is manifested mainly as linear magnetic anomalies, which are caused by granite masses intruded along the large-scale fault belt ( Huang & Wang 1992 ). A recent...
FIGURES | View All (7)
Journal Article
Published: 01 May 1999
Journal of Sedimentary Research (1999) 69 (3): 711–719.
... between the North and South China blocks, suggests that a recycled orogen had never been emplaced in Korea. Reference of the tectonic divisions of Korea to those of China or Japan should be made with substantial care. This includes the current attempts to relate the Imjingang Belt with the Qinling...
Journal Article
Published: 01 March 2014
European Journal of Mineralogy (2014) 26 (1): 5–23.
... and are compared with published P - T estimates. The multi-stage Qinling-Tongbai-Hong’an-Dabie-Sulu-Imjingang orogen stretches more than 2000 km in eastern Asia ( Fig. 1a ) and comprises the Sino-Korean craton in the north, the long and narrow Qinling micro-continent in the center, and the Yangtze...
FIGURES | View All (9)
Journal Article
Journal: Geology
Published: 01 April 1995
Geology (1995) 23 (4): 353–356.
...W. G. Ernst; J. G. Liou Abstract The Dabie Mountains are part of the >2000-km-long Qinling-Dabie-Sulu suture zone juxtaposing the Sino-Korean and Yangtze cratons. An eastern extension apparently crosses Korea and lies along the Japan Sea side of Honshu as the Imjingang and Sangun terranes...
Series: Geological Society, London, Special Publications
Published: 17 April 2019
DOI: 10.1144/SP478.5
EISBN: 9781786204165
.... Fig. 1. The tectonic map of northeastern Asia showing the tectonic relationships between Korea, China and Japan, along with distribution of the Permo-Triassic eclogites (modified after Oh 2006 and Dong et al. 2011 ). IB, Imjingang belt; OMB, Okcheon metamorphic belt; HS, Hongseong area; ODS...
FIGURES | View All (17)
Journal Article
Journal: Geology
Published: 01 April 2003
Geology (2003) 31 (4): 307–310.
... fault divides the Dabie belt to the southwest from its counterpart Sulu belt to the northeast ( Fig. 1 , inset). The latter is known to have lithological features similar to those of the Dabie belt to the west and the Imjingang belt (central Korea) to the east ( Yin and Nie, 1993 ), e.g., the presence...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP338.6
EISBN: 9781862395862
..., then the combined Jiamusi–Khanka terrane is related to circum-Pacific accretion and does not form a microcontinental block that was trapped between the Siberia and North China cratons during the main assembly of the Central Asian Orogenic Belt. We thank A. Frew for assistance with the SHRIMP II data collection...
FIGURES | View All (5)
Image
Schematic geological map of the Dabie-Sulu metamorphic <b>belts</b> including Kore...
Published: 01 December 2014
; IB – Imjingang Belt; OB – Ogcheon Belt; YM – Yeongnam massif (modified after Kim et al. , 2006 ; Li et al. , 2011 ). Lower right inset of Qianliyan Island modified after Han et al. (2007) . (online version in colour)
Series: Geological Society, London, Geology of Series, Geological Society, London, Geology of Series
Published: 01 January 2016
DOI: 10.1144/GOJ.2
EISBN: 9781862397064
... Abstract Pre-Cenozoic rocks of the Japanese islands are largely composed of latest Palaeozoic to Cretaceous accretionary complexes and Cretaceous granitic intrusives. Exposures of older rocks are restricted to a limited number of narrow terranes, notably the Hida, Oeyama and Hida Gaien belts...
FIGURES | View All (28)
Image
Geological sketch map of the Early Precambrian North China Craton and the K...
Published: 01 May 2007
Figure 1. Geological sketch map of the Early Precambrian North China Craton and the Korean Peninsula. NM – Rangnim Massif; IB –Imjingang Belt; GM – Gyeonggi Massif; OB – Ogcheon Belt; YM – Yeongnam Massif; PB – Pyeongnam basin; TB – Taebaek basin.
Image
Average Rayleigh-wave phase velocities at stations in five geologic areas: ...
Published: 01 August 2005
Figure 2. Average Rayleigh-wave phase velocities at stations in five geologic areas: (a) the Imjingang belt, (b) the Gyeonggi massif, (c) the Okcheon belt, (d) the Yeongnam massif, and (e) islands. Symbols and corresponding station names are given in each legend.
Image
Tectonic map of the Korean Peninsula and adjacent area (modified from  Min ...
Published: 01 June 2007
Figure 1. Tectonic map of the Korean Peninsula and adjacent area (modified from Min and Cho, 1998 ; Chough et al. , 2000 ). Major tectonic provinces are separated by dashed lines. NM, Nangrim massif; IB, Imjingang belt; GM, Gyeonggi massif; OB, Okcheon (fold) belt; YM, Yeongnam massif; GB
Image
F ig . 1. Simplified geologic map of the regional geology and location of t...
Published: 01 May 2002
= Imjingang belt; NB = Nangrim block; OB = Ogcheon belt; and YB = Yeongnam block.
Image
Geological map of the Ulsan mine area showing the detailed map of the minin...
Published: 01 June 2000
F ig . 1. Geological map of the Ulsan mine area showing the detailed map of the mining geology. The location of the Ulsan mine area (shaded box) is shown on the inset map of the Republic of Korea. GB: Gyeongsang Basin, GM: Gyeonggi Massif, IB: Imjingang Belt, NM: Nangrim Massif, OB: Ogcheon Belt
Image
( a ) Major tectonic units of East Asia. Inset figure is an enlarged map of...
Published: 01 April 2009
F igure 1. ( a ) Major tectonic units of East Asia. Inset figure is an enlarged map of the Imjingang belt subdividing the Gyeonggi and Nangrim massifs. ( b ) Simplified geological map of the study area, showing the isograds, sample locations, and index mineral assemblages. Abbreviations: GM
Image
(a) Simplified tectonic map of the Sino–Korean Block (yellow colour). Light...
Published: 20 November 2017
Figure 1. (a) Simplified tectonic map of the Sino–Korean Block (yellow colour). Light yellow colour in the Korean Peninsula and Japan represents the tectonic provinces under debate. NM – Nangrim Massif; PB – Pyeongnam Basin; IB – Imjingang Belt; GM – Gyeonggi Massif; OMB – Okcheon Metamorphic
Journal Article
Published: 01 December 2011
Bulletin of the Seismological Society of America (2011) 101 (6): 2819–2832.
...,b ). The Nangrim and Gyeonggi massifs are separated by the Imjingang belt, a narrow suture zone that recorded high-grade metamorphic events in the late Permian–early Triassic ( Cho et al. , 1995 ; Ree et al. 1996 ). The Gyeonggi and Yeongnam massifs are separated by the Okcheon fold belt...
FIGURES | View All (12)