胶东照岛山金矿黄铁矿成分与热电性标型特征研究

对胶东照岛山金矿中黄铁矿成分和热电性标型特征研究表明：黄铁矿成分亏S富As;黄铁矿的特征元素为：As,Co,Ni,Mo,Se,Au,Ag,Sb,Pb,Te,不同成矿阶段微量元素含量的变化说明,黄铁矿的形成温度从早期成矿阶段到主成矿阶段逐渐降低,金沉淀主要发生在石英黄铁矿和多金属硫化物阶段;P型黄铁矿出现率为61%,与胶东几个典型金矿相比,黄铁矿热电系数离散性较大;热电导型按成矿时间先后变化规律为：P〉N→P〈N→P〉〉N→P〉〉N;As是金矿化的有利组分,微量元素As与（Co＋Ni）的相对含量与黄铁矿P型、N型出现率及导型组合密切相关。结合黄铁矿成矿温度、热电系数垂向变化以及黄铁矿P型出现率、P型均值分带性等标型特征的研究表明：照岛山金矿床的形成温度为150℃~340℃,属中低温矿床;矿床总体剥蚀较浅,深部矿体未被揭露;P型黄铁矿热电系数均值、出现率高值区是有利的找矿标志。黄铁矿热电性参数显示,矿区南部矿段（8线~16线）和北部矿段（120线）-200 m以下分别存在一处高值区,推测两处具有深部找矿前景。

胶东牟平照岛山金矿蚀变矿化阶段及控矿要素

照岛山金矿位于胶东牟平-乳山成矿带北段,矿体产于中生代燕山期昆嵛山二长花岗岩中,主要受NNE向金牛山断裂带的控制。对金的成矿背景、矿床地质、控矿因素和矿体隐伏特征的研究结果表明:围岩蚀变从近矿到远矿依次发育黄铁绢英岩化、绢英岩化和钾长石化;金的成矿分为黄铁矿石英、石英黄铁矿、多金属硫化物、石英碳酸盐矿物4个阶段;昆嵛山岩体和荆山群变质岩的接触带附近易于成矿;金牛山主断裂走向NE的拐折地段、不同期次断裂交会处和多期断裂破碎带部位都易于成矿;金品位高值区呈近似等距分布,32线以南有向SW侧伏的趋势,40线以北有向NE侧伏的趋势。总结了照岛山金矿的控矿因素,初步推测了深部找矿方向。

Suitability evaluation of regional coastal ecotourism based on SOM neural network model: a case study of Qingdao, Yantai, Weihai and Rizhao of Shandong Province

Development of coastal ecotourism has been a,focus of Shandong government, and the suitability evaluation of regional eoastai ecotourism is crucial for the reasonable plan and sustainable development of Shandong coastal ecotourism. By using MATLAB language to establish a SOM neural network model, this＇ paper evaluates the eoastal ecotourism suitability of four regions, Qingdao. Yantai, Weihai and Rizhao of Shandong Province and divides 33 subordinate regions of those four cities into four categories, i.e. regions poorly suitable for ecotourism resources, regions highly suitable for coastal ecotourism, regions secondly suitable for coastal ecotourism, regions ordinarily suitable.for coastal ecotourism, Related suggestions on development of regional coastal ecotourism have been given in the final conclusions.