ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    厄立特里亚Kerkebet及邻区地质构造演化及成矿作用简述

    Brief Description of Geological-Tectonic Evolution and Metallogenesis at Kerkebet and Adjacent Areas in Eritrea

    • 摘要: 厄立特里亚Kerkebet勘查区位于努比亚地体内Augaro-Adobha成矿带,成矿条件优越。近年来在该区的找矿勘查取得重大突破,发现评价了Mier中型金矿床。调查显示勘查区内多个目标区(Shukula、Locotat、Yasiney、Koken等)均显示较大的金多金属矿找矿潜力,成矿作用明显受地质构造演化控制。然而,受基础地质调查和综合研究程度限制,该区域尚未开展系统的地质构造演化调查和研究工作,严重制约了区域及Kerkebet勘查区的找矿勘查和理论指导。基于此,笔者通过系统梳理区域及Kerkebet勘查区已有资料,结合野外地质调查研究,采用“多岛弧盆系”构造理论对以往的Nakfa地体重新划分了区域构造单元,划分出①Barka岩浆弧、②Kerkebet俯冲增生杂岩带、③Nakfa岩浆弧等3个一级构造单元;对金多金属矿体主要赋存的Kerkebet俯冲增生杂岩带进一步划分出3个二级构造单元;揭示Kerkebet俯冲增生杂岩带构造演化阶段与不同矿化类型金矿床形成的耦合关系;基于不同的构造单元对应相似的或不同的岩组/段,构建了Kerkebet增生杂岩带构造−地层格架。该区特定矿床具有反映大地构造环境时空专属性的特点,结合区域矿床类型组合及分布情况,构建了该区构造演化−成矿作用模式。研究为深化区域构造−成矿作用理论提供基础依据,为Kerkebet勘查区下一步找矿勘查实践指明方向。

       

      Abstract: Located in the Augaro-Adobha metallogenic belt in the Nubian terrane, the Kerkebet exploration area shows superior metallogenic conditions in Eritrea. Recent years, major breakthroughs have been made in this exploration area, and the Mier medium-sized gold deposit has been found and evaluated. It is also found by field investigation that many target areas (e.g., Shukula, Locotat, Yasiney, Koken et al.) in this area show great gold polymetallic prospecting potential, and the mineralization is obviously controlled by geological-tectonic evolution. However, due to the limitation of previous basic geological survey and comprehensive researches, this region has not yet carried out systematic studies on geological-tectonic evolution, which seriously restricts the prospecting exploration and theoretical guidance. Based on this, after systematically sorting out the existing data of this region, this paper adopts the "multi-island-arc-basin system" tectonic theory to re-divide the previous Nakfa terrane into three new tectonic units (Barka magmatic arc, Kerkebet subduction accretionary complex, and Nakfa magmatic arc), among which the Kerkebet subduction accretionary complex was further divided into three second tectonic units, and reveals the relationship between tectonic evolution stages and different gold deposit types of the Kerkebet subduction accretion complex belt, combined with field investigations and researches. We also construct the tectonic-stratigraphic framework of this region, based on the fact that different tectonic units correspond to similar or different rock groups/segments. According to the fact that specific deposits have the characteristics of reflecting the temporal-spatial specificity of the tectonic environment, we also constructed the tectonic-mineralization model based on regional deposit types and distribution. These researches will not only provide the basis for deepening the theory of regional tectonics-metallogenesis, but also point out the directions for the next prospecting and exploration practice at Kerkebet.

       

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