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Carlin-type Gold Prospects in Surigao del Norte, Mindanao Island, Philippines: Their Geology and Mineralization Potential

机译:菲律宾棉兰老岛苏里高德尔北的卡林型金矿前景:其地质和矿化潜力

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摘要

Three calcareous sedimentary rock-hosted Carlin type-like gold prospects were mapped in a mineral production sharing agreement area of Philex Gold Philippines Inc. in Taganaan municipality, Surigao del Norte province in Mindanao island in the Philippines. They occur along a 20-25 km long trend of known epigenetic gold and porphyry copper deposits that lie close to several splays of the Philippine Fault Zone. The gold district forms part of the Late Cretaceous Eastern Mindanao Range that hosts early Paleogene and late Pliocene to Quaternary intrusive rocks. Gold is invisible in the jasperoid outcrops in Lascogon, Napo, and Danao prospects. The jasperoids occur in lenses of marls belonging to the Taganaan Marl Member that is associated to a turbiditic member of the Middle Miocene Mabuhay Formation. The marl lenses include gently dipping interbedded silty limestones and calcareous shales. The "invisible gold" mineralization in silicified calcareous rocks resembles Carlin-type deposits. Based on the mapped igneous and sedimentary rocks, a possible heat source for the gold mineralization is either or both of the two main phases of intrusion, Mabuhay An-desite or Alipao Andesite Porphyry. Forty-eight rock samples, fifteen stream sediment samples, and one soil sample were critical in delineating the general features of the potential Carlin-type prospects. The gold grades of jasperoids in the three prospects range from trace amounts to 20 g/t Au. Regional studies of gold and porphyry copper mineralization in the Surigao del Noite mineral district are important in delineating ore targets for drilling in the three prospects.
机译:在菲律宾棉兰老岛苏里高德尔省北塔加纳市的菲莱克斯黄金菲律宾公司的矿产生产共享协议区域中,绘制了三个钙质沉积岩类卡林型金矿前景图。它们沿着已知表观生金和斑岩铜矿床的20-25公里长的趋势发生,这些矿床与菲律宾断层带的几个张开接近。金矿区是棉兰老岛晚白垩世山脉的一部分,该山脉拥有古近纪晚期和上新世晚期至第四纪侵入岩。在Lascogon,Napo和Danao等地区的碧玉露头中看不见黄金。碧玉出现在属于Taganaan Marl成员的泥灰岩中,该泥岩与中新世中部Mabuhay组的湍流成员相关。泥灰岩镜片包括轻轻浸入层间的粉质灰岩和钙质页岩。硅质钙质岩石中的“无形金”矿化类似于卡林型矿床。根据测绘的火成岩和沉积岩,金矿化的可能热源是侵入的两个主要阶段中的一个或两个,即Mabuhay An-desite或Alipao Andesite斑岩。 48个岩石样品,15个河流沉积物样品和1个土壤样品对于描述潜在的卡林型勘探区的总体特征至关重要。在这三个矿床中,金碧玉的品位范围从痕量到20 g / t Au。 Surigao del Noite矿区的金矿和斑岩铜矿化的区域研究对于确定三个前景中的钻探矿石目标至关重要。

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