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A Proposal of Caldera‐Related Genesis for the Roseki Deposits in the Mitsuishi Mining Area, Southwest Japan
Author(s) -
ISHIHARA Shunso,
IMAOKA Teruyoshi
Publication year - 1999
Publication title -
resource geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.597
H-Index - 43
eISSN - 1751-3928
pISSN - 1344-1698
DOI - 10.1111/j.1751-3928.1999.tb00041.x
Subject(s) - caldera , geology , rhyolite , geochemistry , volcano , pyrophyllite , breccia , basement , petrology , geomorphology , seismology , paleontology , volcanic rock , archaeology , history
Geology of the largest Roseki (pyrophyllite–clay)–mineralized, Mitsuishi mining area was re–examined, and a composite caldera model (Wake caldera) was proposed. Evidence for the caldera formation is (1) Existence of huge volume of rhyolitic tuffs in the mining area, (2) A basin structure in rhyolitic tuffs surrounded by the Permo‐Triassic basement rocks, (3) Arc‐like distribution of the Roseki deposits along the eastern edge of the proposed caldera, (4) Tectonic disturbance and intrusive bodies along the caldera wall, and (5) Presence of meso– and mega‐breccias at the bottom of the caldera wall. The proposed caldera, sizing NNW‐SSE 23 km by ENE‐WSW 15 km, may have younger, Inner caldera (15 by 15 km), defined by Lower Member of the late Cretaceous rhyolitic tuffs, thus composite in character. The Roseki deposits were formed after the Inner caldera collapse by hydrothermal fluids ascended through the caldera wall, then spread into the permeable horizon. This caldera proposal bears a significant change in the regional exploration strategy for the Roseki deposits.