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학술저널

平昌-旌善一帶의 地質構造 糾明

On the geologic structure of Pyeongchang-Jeongseon area

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By the present study on the geological structure of the area, it becomes clear at the formations known as the Jeongseon, Pyeongchang, and Yeongweol types of the Joseon System are no more than the structural repetitions of the Duwibong type of the System, and that the so far known thrust fault in the area is merely a overturned anticline associated with some displacement along the axial plane.

Abstract

1. 緖言

2. 本域에 發達된 朝鮮系의 各型에 關한 從來의 見解

3. 本域의 橫造에 關한 從來의 見解와 이에 對한 反證

4. 本域의 地質構造에 關한 새로운 解釋

5. 層序에 關한 새로운 解釋

6. 本域의 構造

7. 結語

參考文獻

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