琵琶湖周辺の花崗岩類

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書誌事項

タイトル別名
  • Granitic masses around Lake Biwa, southwest Japan
  • 琵琶湖周辺の花崗岩類-2-鈴鹿花崗岩体
  • ビワコ シュウヘン ノ カコウガンルイ 2 スズカ カコウガンタイ
  • その2 鈴鹿花崗岩体
  • Part 2: The Suzuka Granite pluton

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抄録

The Suzuka Granite pulton occupies the backborn area of the Suzuka Mountains, southwest Japan. It has an extent of 3〜9km (E-W)×13km (E-S), convex by arched southeastward, being intruded into the late-Paleozoic to Mesozoic formations of the Mino belt. The northern half of the pulton consists of biotite granites of following three major rock-types, the Yunoyama-type, Happudani-type and Kanzaki-type, and subordinate Hatomine-type. Two intrusive stages are recognized for them. The Suzuka Granite is associated with the porphyries, which are related to the late-Cretaceous felsic volcanism (Koto Rhyolites) forming a cauldron. The Suzuka Granite is considered to an outer most part of the ring complex in the south of Lake Biwa.

収録刊行物

  • 地球科学

    地球科学 44 (4), 184-195, 1990

    地学団体研究会

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