Paleoproterozoic orogeny in South Korea

Evidence from Sm-Nd and Pb step-leaching garnet ages of Precambrian basement rocks

Hee Sagong, Chang Sik Cheong, Sung Tack Kwon

Research output: Contribution to journalArticle

76 Citations (Scopus)

Abstract

Geology and tectonics of the Korean Peninsula have been considered to be closely associated with those of the adjacent Chinese continent. Although Phanerozoic connections between the two areas have been reasonably well worked out, Precambrian ones are less well established. We obtained Sm-Nd and U-Pb garnet ages of 12 metamorphic rocks from widely separated parts of the Gyeonggi and Yeongnam massifs in South Korea to better understand their Precambrian history. The two massifs consist of late Archean to Paleoproterozoic basement rocks and Meso- to Neoproterozoic supracrustal rocks. Previous studies have shown that the two massifs experienced upper amphibolite to granulite facies metamorphism of medium pressure type with clockwise P-T-time paths, suggesting that the two massifs may represent remnants of a collisional orogen. Pb-Pb and U-Pb garnet ages give two distinct age groups: ten Paleoproterozoic (1989 ± 34 to 1835 ± 56 Ma) ages of basement rocks from the two massifs, and one late Permian (265 ± 8 Ma) age of a supracrustal rock from the Gyeonggi massif that corroborates previous estimates of Permo-Triassic (298-245 Ma) metamorphic age for the supracrustal rocks. On the other hand, Sm-Nd garnet ages are less precise and display a wide range of ages from 2257 to 413 Ma for the basement rocks. When we compare the Sm-Nd and Pb-Pb ages from the same sample, the Sm-Nd age is similar to or younger than the Pb-Pb age, suggesting that the blocking temperature of the Sm-Nd garnet system may be lower than that of the U-Pb system (>800°C). We interpret the Pb-Pb and U-Pb ages as representing the timing of metamorphic garnet growth, since the blocking temperature of the U-Pb garnet system is similar to or higher than the metamorphic temperature of the analyzed samples. Apparently, the younger metamorphism, possibly associated with the Permo-Triassic collision between the North and South China cratons, was not strong enough to reset the older metamorphic age. Similar Paleoproterozoic metamorphic ages for basement rocks of the two massifs suggest that they may have come from the same Precambrian terrane. The metamorphic ages of the basement rocks of South Korea agree very well with those of the Central Zone (orogenic belt) in the North China craton, suggesting a possible correlation between the two terranes.

Original languageEnglish
Pages (from-to)275-295
Number of pages21
JournalPrecambrian Research
Volume122
Issue number1-4
DOIs
Publication statusPublished - 2003 Apr 10

Fingerprint

Garnets
basement rock
orogeny
Leaching
Precambrian
garnet
Rocks
leaching
supracrustal rock
Metamorphic rocks
Tectonics
Geology
Temperature
craton
terrane
metamorphism
Triassic
temperature
granulite facies
amphibolite

All Science Journal Classification (ASJC) codes

  • Geochemistry and Petrology
  • Geology

Cite this

@article{a5f9d2daa1fc4fe5a5c4c0591ab96c4e,
title = "Paleoproterozoic orogeny in South Korea: Evidence from Sm-Nd and Pb step-leaching garnet ages of Precambrian basement rocks",
abstract = "Geology and tectonics of the Korean Peninsula have been considered to be closely associated with those of the adjacent Chinese continent. Although Phanerozoic connections between the two areas have been reasonably well worked out, Precambrian ones are less well established. We obtained Sm-Nd and U-Pb garnet ages of 12 metamorphic rocks from widely separated parts of the Gyeonggi and Yeongnam massifs in South Korea to better understand their Precambrian history. The two massifs consist of late Archean to Paleoproterozoic basement rocks and Meso- to Neoproterozoic supracrustal rocks. Previous studies have shown that the two massifs experienced upper amphibolite to granulite facies metamorphism of medium pressure type with clockwise P-T-time paths, suggesting that the two massifs may represent remnants of a collisional orogen. Pb-Pb and U-Pb garnet ages give two distinct age groups: ten Paleoproterozoic (1989 ± 34 to 1835 ± 56 Ma) ages of basement rocks from the two massifs, and one late Permian (265 ± 8 Ma) age of a supracrustal rock from the Gyeonggi massif that corroborates previous estimates of Permo-Triassic (298-245 Ma) metamorphic age for the supracrustal rocks. On the other hand, Sm-Nd garnet ages are less precise and display a wide range of ages from 2257 to 413 Ma for the basement rocks. When we compare the Sm-Nd and Pb-Pb ages from the same sample, the Sm-Nd age is similar to or younger than the Pb-Pb age, suggesting that the blocking temperature of the Sm-Nd garnet system may be lower than that of the U-Pb system (>800°C). We interpret the Pb-Pb and U-Pb ages as representing the timing of metamorphic garnet growth, since the blocking temperature of the U-Pb garnet system is similar to or higher than the metamorphic temperature of the analyzed samples. Apparently, the younger metamorphism, possibly associated with the Permo-Triassic collision between the North and South China cratons, was not strong enough to reset the older metamorphic age. Similar Paleoproterozoic metamorphic ages for basement rocks of the two massifs suggest that they may have come from the same Precambrian terrane. The metamorphic ages of the basement rocks of South Korea agree very well with those of the Central Zone (orogenic belt) in the North China craton, suggesting a possible correlation between the two terranes.",
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Paleoproterozoic orogeny in South Korea : Evidence from Sm-Nd and Pb step-leaching garnet ages of Precambrian basement rocks. / Sagong, Hee; Cheong, Chang Sik; Kwon, Sung Tack.

In: Precambrian Research, Vol. 122, No. 1-4, 10.04.2003, p. 275-295.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Paleoproterozoic orogeny in South Korea

T2 - Evidence from Sm-Nd and Pb step-leaching garnet ages of Precambrian basement rocks

AU - Sagong, Hee

AU - Cheong, Chang Sik

AU - Kwon, Sung Tack

PY - 2003/4/10

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N2 - Geology and tectonics of the Korean Peninsula have been considered to be closely associated with those of the adjacent Chinese continent. Although Phanerozoic connections between the two areas have been reasonably well worked out, Precambrian ones are less well established. We obtained Sm-Nd and U-Pb garnet ages of 12 metamorphic rocks from widely separated parts of the Gyeonggi and Yeongnam massifs in South Korea to better understand their Precambrian history. The two massifs consist of late Archean to Paleoproterozoic basement rocks and Meso- to Neoproterozoic supracrustal rocks. Previous studies have shown that the two massifs experienced upper amphibolite to granulite facies metamorphism of medium pressure type with clockwise P-T-time paths, suggesting that the two massifs may represent remnants of a collisional orogen. Pb-Pb and U-Pb garnet ages give two distinct age groups: ten Paleoproterozoic (1989 ± 34 to 1835 ± 56 Ma) ages of basement rocks from the two massifs, and one late Permian (265 ± 8 Ma) age of a supracrustal rock from the Gyeonggi massif that corroborates previous estimates of Permo-Triassic (298-245 Ma) metamorphic age for the supracrustal rocks. On the other hand, Sm-Nd garnet ages are less precise and display a wide range of ages from 2257 to 413 Ma for the basement rocks. When we compare the Sm-Nd and Pb-Pb ages from the same sample, the Sm-Nd age is similar to or younger than the Pb-Pb age, suggesting that the blocking temperature of the Sm-Nd garnet system may be lower than that of the U-Pb system (>800°C). We interpret the Pb-Pb and U-Pb ages as representing the timing of metamorphic garnet growth, since the blocking temperature of the U-Pb garnet system is similar to or higher than the metamorphic temperature of the analyzed samples. Apparently, the younger metamorphism, possibly associated with the Permo-Triassic collision between the North and South China cratons, was not strong enough to reset the older metamorphic age. Similar Paleoproterozoic metamorphic ages for basement rocks of the two massifs suggest that they may have come from the same Precambrian terrane. The metamorphic ages of the basement rocks of South Korea agree very well with those of the Central Zone (orogenic belt) in the North China craton, suggesting a possible correlation between the two terranes.

AB - Geology and tectonics of the Korean Peninsula have been considered to be closely associated with those of the adjacent Chinese continent. Although Phanerozoic connections between the two areas have been reasonably well worked out, Precambrian ones are less well established. We obtained Sm-Nd and U-Pb garnet ages of 12 metamorphic rocks from widely separated parts of the Gyeonggi and Yeongnam massifs in South Korea to better understand their Precambrian history. The two massifs consist of late Archean to Paleoproterozoic basement rocks and Meso- to Neoproterozoic supracrustal rocks. Previous studies have shown that the two massifs experienced upper amphibolite to granulite facies metamorphism of medium pressure type with clockwise P-T-time paths, suggesting that the two massifs may represent remnants of a collisional orogen. Pb-Pb and U-Pb garnet ages give two distinct age groups: ten Paleoproterozoic (1989 ± 34 to 1835 ± 56 Ma) ages of basement rocks from the two massifs, and one late Permian (265 ± 8 Ma) age of a supracrustal rock from the Gyeonggi massif that corroborates previous estimates of Permo-Triassic (298-245 Ma) metamorphic age for the supracrustal rocks. On the other hand, Sm-Nd garnet ages are less precise and display a wide range of ages from 2257 to 413 Ma for the basement rocks. When we compare the Sm-Nd and Pb-Pb ages from the same sample, the Sm-Nd age is similar to or younger than the Pb-Pb age, suggesting that the blocking temperature of the Sm-Nd garnet system may be lower than that of the U-Pb system (>800°C). We interpret the Pb-Pb and U-Pb ages as representing the timing of metamorphic garnet growth, since the blocking temperature of the U-Pb garnet system is similar to or higher than the metamorphic temperature of the analyzed samples. Apparently, the younger metamorphism, possibly associated with the Permo-Triassic collision between the North and South China cratons, was not strong enough to reset the older metamorphic age. Similar Paleoproterozoic metamorphic ages for basement rocks of the two massifs suggest that they may have come from the same Precambrian terrane. The metamorphic ages of the basement rocks of South Korea agree very well with those of the Central Zone (orogenic belt) in the North China craton, suggesting a possible correlation between the two terranes.

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