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991.
Akira IMAI 《Resource Geology》2000,50(1):1-23
Abstract: The Mamut deposit of Sabah, East Malaysia, is a porphyry type Cu‐Au deposit genetically related to a quartz monzonite (“adamellite”) porphyry stock associated with upper Miocene Mount Kinabalu plutonism. The genesis of the Mamut deposit is discussed based on petrology of the intrusives in the Mount Kinabalu area combined with ore– and alteration–petrography, fluid inclusion and sulfur isotope studies. Groundmass of the adamellite porphyry at Mamut is rich in K which suggests vapor transport of alkaline elements during the mineralizing magmatic process, while the groundmass of the post‐ore “granodiorite” porphyry at Mamut contains small amounts of normative corundum suggesting depletion in alkaline elements at the root zone of the magma column. Sub‐dendritic tremolitic amphibole rims on hornblende phenocrysts in the Mamut adamellite porphyry suggest interaction between the mineralizing magma and the exsolved fluids. Occurrences of clinopyroxene microphenocrysts and pseudomor‐phic aggregates of shredded biotite and clinopyroxene after hornblende phenocrysts in the barren intrusives imply lower water fugacity and decreasing in water fugacity, respectively. Compositional gap between the core of hornblende phenocrysts and the tremolitic amphibole rims and those in the groundmass of the Mamut adamellite porphyry suggests a decrease in pressure. Higher XMg (=Mg/(Mg+Fe) atomic ratio) in the tremolitic amphibole rims in the Mamut adamellite porphyry compared to those of the barren intrusions suggests high oxygen fugacity. High halogen contents of igneous hydrous minerals such as amphiboles, biotite and apatite in the Mamut adamellite porphyry suggest the existence of highly saline fluids during the intrusion and solidification of the mineralizing magma. Fluid inclusions found in quartz veinlet stockworks are characterized by abundant hypersaline polyphase inclusions associated with subordinate amounts of immiscible gaseous vapor. Both Cu and Au are dispersed in disseminated and quartz stockwork ores. Chalcopyrite and pyrrhotite as well as magnetite are the principal ore minerals in the biotitized disseminated ores. Primary assemblage of intermediate solid solution (iss) and pyrrhotite converted to the present assemblage of chalcopyrite and pyrrhotite during cooling. Subsequent to biotitization, quartz veinlet stockworks formed associated with retrograde chlorite alteration. The Cu‐Fe sul–fides associated with stockwork quartz veinlet are chalcopyrite and pyrite. Overlapping Pb and Zn and subsequent Sb mineralizations were spatially controlled by NNE‐trending fractures accompanying the phyllic and advanced argillic alteration envelope. Sulfur isotopic composition of ore sulfides are homogeneous (about +2%) throughout the mineralization stages. These are identical to those of the magmatic sulfides of Mount Kinabalu adamellitic rocks. 相似文献
992.
基于分形理论的SAR图像边缘检测 总被引:2,自引:0,他引:2
分析了SAR图像的基本特点 ,阐述用DFBR模型表达SAR图像的基本原理 ,提出两种基于分形理论的SAR图像边缘检测方法。通过对传统方法、分形方法和多尺度分形方法的特性分析和实验 ,说明分形方法有较强的抗干扰性能 ,适用于SAR图像的边缘检测 ,并且基于多重分形的方法能获得更好的检测结果 相似文献
993.
根据台网布局和实际使用参数,运用反推方法,对大同数字遥测地震台网和模拟遥测地震台网的监控能力进行了计算分析,粗定了数字台网速报表任区的范围,并对数字台网的大震响应能力进行了讨论,结果表明,大同数字台网的监控能力较模拟台网有了较大的提高,整个网内及网缘地震的监控能力为2.0级,网内大部分区域及东部网缘区域可达1.5级;数字台网对网内最大的测定能力为5.0级,网内南部区域可达5.5级;对于网内更大震级的地震,记录将全部限幅,测定震级困难,对山西北部5.5级以上地震要靠山西台网中北部台站来控制。 相似文献
994.
995.
矿井电穿透方法技术的研究 总被引:7,自引:2,他引:5
通过研究工作面两巷道间电穿透建场理论和方法技术,优化出单极—偶极法等6种电穿透技术,用于探测工作面顶底板内的电性变化;煤层偶极—偶极法用于探测工作面煤层内的电性变化,为分别探测工作面顶底板内和煤层内的含、导水构造提供了一套新技术。 相似文献
996.
本文以马坑铁矿浅部矿床为例,论述了矿床技术经济评价的基本方法。作者的研究表明,马坑铁矿浅部矿床的开发建设,在地质上是可能的,技术和经济上也是可行,合理的。 相似文献
997.
998.
在高级变质区会全栈“穹形构造”西缘“线性构造矿源域”基础上,经过古生代,特别是中生代的构造-岩浆作用改造叠加,在王家店花岗岩体风部、边缘、岩体之外,形成岩浆期后热液型金矿,其深部潜在远景有待进一步研究。 相似文献
999.
Hydrochemical characterization of acute acid mine drainage at Iron Duke mine, Mazowe, Zimbabwe 总被引:8,自引:0,他引:8
Acid mine drainage (AMD) with a minimum pH of 0.52 was recorded at Iron Duke mine near Mazowe, Zimbabwe during an investigation
of the environmental geochemistry of mine waters in the Greenstone Belts of Zimbabwe. Hydrochemical data for waters emanating
from the Iron Duke waste-rock pile indicate their super-saturation with respect to Fe and SO4
2–. Extremely high dissolved concentrations of Al, Zn, Cu, Co, Ni, V, Cr, Cd and As also prevail. Substantial losses of metals
from solution occur within 400 m of the AMD source through the precipitation of crystalline sulphates, principally melanterite.
Further downstream, hydrous oxide precipitation forms the dominant mechanism of metal attenuation in waters characteristically
under-saturated with respect to Fe sulphates. Speciation and saturation index data generated using the equilibrium model WATEQ4F,
suggest that such codes have broad utility for generic prediction of the mineralogical contraints on metal mobility in acute
AMD systems. Major discrepancies between modelled and empirical hydrochemistries are, however, evident for super-saturated
waters in which the kinetics of Fe precipitation are slow, and in which total ionic strengths markedly exceed their theoretical
maximum.
Received: 28 August 1998 · Accepted: 7 December 1998 相似文献
1000.
地震勘探技术在石膏矿开发中的应用 总被引:3,自引:0,他引:3
在国内首次将地震勘探技术系统地应用于石膏矿床的开发,控制了石膏层赋存状况和构造特征,获得了较为理想的地质效果和经济效益。 相似文献