岐阜県岩村盆地の新生代層

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概要

• 論文の詳細を見る

• The stratigraphic succession of the Cenozoic strata developed in the Iwamura basin is as follows; Age Terrace deposits unconformity Hirooka gravel Tazawa sand and gravel I_2 Seto group Higashihora formation H_2 Mizunami group Toyama formation Agi formation F_2〜F_3 unconformity and fault Granite and Quartz-porphyry The Mizunami group represents a cycle of sedimentation and its lower part or the Agi formation may be freshwater in origin while the upper or Toyama formation, which consists of five members is marine., The Mizunami group is probably middle Miocene (F_2〜F_3) in age as inferred from the molluscan fossils., It forms a synclinal structure controlled by the fault of NE-WS trend.,

• 日本地質学会の論文
• 1955-11-25

著者

• 糸魚川 淳二

  京都大学理学部地質学鉱物学教室

関連論文

• 岐阜県岩村盆地の新生代層
• Katelysia (Nipponomarcia) nakamurai Ikebe の変異について

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