海南岛石碌铁矿含矿岩系中火山岩类的新发现与究研

NEW DISCOVERY OF VOLCANIC ROCKS IN ORE-BEARING ROCK SERIES IN THE SHILU IRON DEPOSIT ON HAINAN ISLAND

摘要: 在石碌群主要含矿层及主矿层底部发现火山凝灰岩,经过野外工作和深入研究,提出石碌铁矿床的主要矿质来源可能是海底近源火山喷发作用的看法。

Abstract: Since the 1970’s,there have appeared a lot of views about the source of ore substances in the Shilu deposits on Hainan Island.Since 1983,the author and his colleagues have found two layers of volcanic turfs in Bed No.6 that is the main ore-bearing bed in the Shilu Group,and found volcanic tuff layers at a few localities in the upper part of the schist of Bed No.5 at the base of the principal ore bed,A unit of low-grade volcanic-sedimentary clastic rocks with lenticular volcanic lavas and volcanic tuff has been tentatively defined in the middle-upper parts of Bed No.5.They discovered diopside rocks in the cross section of volcanic rocks and not devitrified volcanic glass in altered diopside dolomite.Therefore it is proposed that the ore substances of the Shilu iron deposit might originate mainly from submarine proximal volcanic eruption.