摘要
通过对区域地形形态、地质构造格架、大厂矿田的矿床地质、地球化学特征的研究,阐明了大厂矿区所处的构造位置为一盆-山构造系。大厂锡石多金属硫化物矿床的生成、发展和演化是该盆一山构造系发展演化的产物,受盆-山构造系的控制。本矿床按矿体形态、矿床特征可以分为层状矿化和脉状矿化两大类。层状矿化是盆-山构造系形成早期同生沉积的,严格受地层层位和岩性的控制。脉状矿化是盆-山构造系发展演化的晚期不同阶段中受岩浆热液作用的叠加、改造而成,受构造和层位的双重控制。
The paper studies the original geography, tectonic framework, geology and geochemisry of the Dachang tin-polymetallic ore field. The ore field is located in a basin-and-range tectonic system. Formation, development and evolution of the ore deposits are mainly controlled by the basin-and-range tectonic system.According to ore body topography and mineralization features, the ore deposits can be divided into 2 mineralization types, stratiform and vein types. The stratiform mineralization which is controlled by stratigraphic sequence and lithology can be formed by sedimentation in the early stage of the basin-and-range system, and the vein mineralization which is controlled by both the fault and stratigraphic sequence can be due to magmatic hydrothermal overprint and reformation for primary mineralizational strata.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1998年第4期332-338,共7页
Geotectonica et Metallogenia
基金
国家自然科学基金
关键词
盆-山构造系
多金属矿床
锡石
锡矿床
成矿作用
Basin-and-range tectonic system, Dachang tin ore held, middle-crustplastic zone