Reply to comment by Y. Park and J.-H. Ree on 'Chemical remagnetization of the Upper Carboniferous-Lower Triassic Pyeongan Supergroup in the Jeongseon area, Korea: fluid migration through the Ogcheon Fold Belt'
- Authors
- Park, Yong-Hee; Doh, Seong-Jae; Suk, Dongwoo
- Issue Date
- Oct-2006
- Publisher
- Geological Society by Blackwell Scientific
- Keywords
- chemical remagnetization; fluid migration; Korea; palaeomagnetism
- Citation
- Geophysical Journal International, v.167, no.1, pp.20 - 23
- Indexed
- SCIE
SCOPUS
- Journal Title
- Geophysical Journal International
- Volume
- 167
- Number
- 1
- Start Page
- 20
- End Page
- 23
- URI
- https://scholarworks.bwise.kr/erica/handle/2021.sw.erica/44654
- DOI
- 10.1111/j.1365-246X.2006.03048.x
- ISSN
- 0956-540X
- Abstract
- In their comment, Park & Ree have raised several points against the interpretation by Park et al., and argued that the remagnetization in the Jeongseon area was caused by the thermal effects of a Late Cretaceous pluton and/or associated short-range hydrothermal fluids, rather than by long-range fluids advocated by us. We disagree with most points raised by Park & Ree and we make a case that these are invalid because of what we believe is incorrect geologic evidence. Hence, our model-that the fluids causing the chemical remagnetization might migrate through the fault system within the Ogcheon Fold Belt-is the most plausible scenario. We recognize that our model needs to be tested in a future study and we welcome new interpretations for or against our model based on reliable geologic or geophysical data.
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