• Proceedings of the KSEEG Conference
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• 2000.04b
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• pp.276-277
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• 2000

• The Korean Journal of Petroleum Geology
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• v.3 no.1 s.4
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• pp.28-39
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• 1995

The objective of this study is to investigate the origin of the dolomite in the Pungchon Formation of the Choseon Supergroup near Taebaeg City, Kangwondo, Korea. The Pungchon Formation is composed of limestone, dolomitic limestone, and dolomite with thin beds of flat pebble conglomerate (FPC) and mudrock. Texturally, the dolomite in the Pungchon Formation can be divided into four types; 1) coarse-sized, xenotopic dolomite in massive dolomite, 2) medium-siEed, idiotopic dolomite in flat pebble conglomerate, 3) xenotopic dolomite replacing ooids, algalnodules, and echinoderms, and 4) the dolomite in mottled fabric. The dolomite in mottled fabric can be subdivided into three types; a) coarse-sized, xenotopic saddle dolomite cement, b) medium-sized, idiotopic, cloudy-centered, clear-rimmed (CCCR) dolomite, and c) coarse-sized, idiotopic dolomite. The carbon isotopic composition of the Pungchon dolomite is in the range of $-2.8-1.4\%_{\circ}(PBD)$, suggesting that the carbon isotopic composition was buffered by the preexisting marine carbonates. Lighter oxygen isotopic values ($\delta^{18}O-15.7-8.7\%_{\circ}, PBD$) indicate that the Pungchon dolomite may have formed under high temperature in a burial diagenetic environment. The higher initial $^{87}Sr/^{86}Sr$ ratio of the Pungchon dolomite (0.7010-0.7161) than that of the coeval Cambrian seawater (0.7088-0.7092) indicates that dolomitizing fluids had been modified from the isotopic exchange with continental crust. Low Sr and Na contents(<200 ppm) of dolomite agree well with previously reported data for burial dolomite. Hifh Fe and Mn contents of the dolomite support the idea that the Pungchon dolomite may have formed in a deep burial diagenetic environment.

• Korean Journal of Materials Research
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• v.7 no.2
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• pp.157-161
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• 1997

The crystallographic site dependent substitution of $^{18}O$ for $^{16}O$ in $Bi_{2}Sr_{2}Ca_{0.8}Y_{0.2}Cu_{2}^{16}O_{8+\delta}$ has heen investigated. In the Kaman spectra of $Bi_{2}Sr_{2}Ca_{0.8}Y_{0.2}Cu_{2}^{16}O_{8+\delta}$ three prominent Raman bands are observed at 297. 464, and $623cm^{-1}$. As the $^{16}O$ arc replaced hy $^{18}O$, all the three bands shift to lower wavewnumbers. The rate of this isotopic shift is similar for the hands at 397 and $464cm^{-1}$. whereas it is quite slower for the hand at $623cm^{-1}$ '['his implys that the $^{16}O-^{18}O$ exchange reaction is crystallographic sites dependent. .Assuming a tetragonal symmetry, we assign the bands at 623. 464, and $297cm^{-1}$ to the vibrations of $O_{pl}(A_{g}),\;O_{ap}\;and\;O_{Bi}$ respectively.