Abstract
The Upper Carboniferous-Lower Triassic Pyongan Supergroup is exposed in an E-W trending syncline comprising the Samcheok Coalfield in eastern South Korea. Although a Recent field overprint widely recorded in Korean rocks is represented here, an ancient field component structure is recovered from red bed facies. A prominent Upper Jurassic-Cretaceous overprint is widespread and records the magnetic effect of the Daebo Orogeny within the Okcheon Belt. Components predating this deformation are recovered from the Lower Triassic, Permian and Upper Carboniferous sediments. A first-order correlation is identified between the Korean Peninsula and North China at least since Upper Paleozoic times. Establishment of, and movements along, the Tan Lu Fault System since Mesozoic times have not obscured this palaeomagnetic correlation. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 850-863 |
| Number of pages | 14 |
| Journal | Geophysical Journal International |
| Volume | 117 |
| Issue number | 3 |
| Publication status | Published - 1994 Jan 1 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Palaeomagnetism of the (Upper Palaeozoic-Lower Mesozoic) Pyongan Supergroup, Korea : a Phanerozoic link with the North China Block. / Doh, Seong-Jae; Piper, J. D A.
In: Geophysical Journal International, Vol. 117, No. 3, 01.01.1994, p. 850-863.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Palaeomagnetism of the (Upper Palaeozoic-Lower Mesozoic) Pyongan Supergroup, Korea
T2 - a Phanerozoic link with the North China Block
AU - Doh, Seong-Jae
AU - Piper, J. D A
PY - 1994/1/1
Y1 - 1994/1/1
N2 - The Upper Carboniferous-Lower Triassic Pyongan Supergroup is exposed in an E-W trending syncline comprising the Samcheok Coalfield in eastern South Korea. Although a Recent field overprint widely recorded in Korean rocks is represented here, an ancient field component structure is recovered from red bed facies. A prominent Upper Jurassic-Cretaceous overprint is widespread and records the magnetic effect of the Daebo Orogeny within the Okcheon Belt. Components predating this deformation are recovered from the Lower Triassic, Permian and Upper Carboniferous sediments. A first-order correlation is identified between the Korean Peninsula and North China at least since Upper Paleozoic times. Establishment of, and movements along, the Tan Lu Fault System since Mesozoic times have not obscured this palaeomagnetic correlation. -from Authors
AB - The Upper Carboniferous-Lower Triassic Pyongan Supergroup is exposed in an E-W trending syncline comprising the Samcheok Coalfield in eastern South Korea. Although a Recent field overprint widely recorded in Korean rocks is represented here, an ancient field component structure is recovered from red bed facies. A prominent Upper Jurassic-Cretaceous overprint is widespread and records the magnetic effect of the Daebo Orogeny within the Okcheon Belt. Components predating this deformation are recovered from the Lower Triassic, Permian and Upper Carboniferous sediments. A first-order correlation is identified between the Korean Peninsula and North China at least since Upper Paleozoic times. Establishment of, and movements along, the Tan Lu Fault System since Mesozoic times have not obscured this palaeomagnetic correlation. -from Authors
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UR - http://www.scopus.com/inward/citedby.url?scp=0028323896&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0028323896
VL - 117
SP - 850
EP - 863
JO - Geophysical Journal International
JF - Geophysical Journal International
SN - 0956-540X
IS - 3
ER -