新疆雅满苏东南河铁矿地质特征及成矿规律研究
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摘要
为了正确地推测新疆雅满苏东南河地区矿体形态、产状及延伸,确保有效对该地区进行实际地质勘查,对雅满苏东南河地区铁矿地质特征及成矿规律进行了研究。研究得出:矿体赋存于黑云斜长片麻岩、白云石大理岩中,从而在勘查工作中,沿黑云斜长片麻岩、白云石大理岩布置工程,确立勘察方向;根据岩石断层擦痕以及产状倾向和走向,在勘查过程中,判定矿体呈"豆角状"或"扁担状"向南东方向侧伏,因此在部署钻探工程时,根据勘查线离矿体露头远近设计调整不同钻孔深度,从而减少工程量,有效指导地质勘探工作的布局。
In order to correctly estimate the ore body shape,occurrence and extension of the ore body in the Yannong southeastern region of Xinjiang,to ensure the effective geological survey of the area,the geological characteristics and metallogenic regularity of the iron ore in the southeast of the Yalong Su Dongan River were studied.The study shows that the orebody is found in the black marble slender gneiss and dolomite marble,so that in the exploration work,along the black skewed gneiss,dolomite marble layout project,to establish the direction of investigation; Rock fault scratches and the tendency and direction of production,in the exploration process,to determine the ore body was " bean-shaped" or " flat-like" to the south-east side of the side,so the deployment of drilling works,according to the exploration line from the ore outcrop distance design to adjust the depth of different drilling,thereby reducing the amount of engineering,and effectively guide the layout of geological exploration work.
In order to correctly estimate the ore body shape,occurrence and extension of the ore body in the Yannong southeastern region of Xinjiang,to ensure the effective geological survey of the area,the geological characteristics and metallogenic regularity of the iron ore in the southeast of the Yalong Su Dongan River were studied.The study shows that the orebody is found in the black marble slender gneiss and dolomite marble,so that in the exploration work,along the black skewed gneiss,dolomite marble layout project,to establish the direction of investigation; Rock fault scratches and the tendency and direction of production,in the exploration process,to determine the ore body was " bean-shaped" or " flat-like" to the south-east side of the side,so the deployment of drilling works,according to the exploration line from the ore outcrop distance design to adjust the depth of different drilling,thereby reducing the amount of engineering,and effectively guide the layout of geological exploration work.
引文
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[2]王惠江,朱余银,樊文军.新疆东南河铁矿地质特征及矿床类型[J].新疆有色金属,2014(B05):42-44.
[3]吴飞,张亮,齐利平,等.新疆哈密市碧玉铜多金属矿地质特征及成矿规律[J].西部探矿工程,2017,29(8):162-165.
[4]易华,赵莉.新疆哈密市雅满苏铁矿地质特征的分析与问题研究[J].中国科技博览,2014(3):348.
[5]曾红.新疆东天山雅满苏铁矿矽卡岩研究及矿床成因探讨[D].乌鲁木齐:新疆大学,2015.
[6]曾红,柴凤梅,周刚,等.新疆雅满苏铁矿床矽卡岩和磁铁矿矿物学特征及其地质意义[J].中国地质,2014(6):1914-1928.
[7]丁建华,李厚民,李立兴,等.新疆雅满苏铁矿区碳酸盐岩地质地球化学特征及其对矿床成因的制约[J].矿床地质,2017,36(1):219-236.
[8]王建设.新疆哈密东戈壁-雅满苏地区区域地质特征及成矿条件分析[D].乌鲁木齐:新疆大学,2015.
[9]姜福芝,秦克章,方同辉,等.东天山铁矿床类型、地质特征、成矿规律与找矿方向[J].新疆地质,2002,20(4):379-383.
[10]丁天府.新疆雅满苏组层控型铁矿的地质特征[J].地质通报,1990(3):79-82.
[11]徐友宁.新疆鄯善百灵山地区铁矿床地质特征及成因探讨[D].西安:长安大学,1996.
[12]曾红,周刚,柴凤梅,等.新疆雅满苏磁铁矿床成矿流特征研究[J].矿床地质,2014(s1):593-594.
[13]卢登蓉,姬金生,吕仁生,等.新疆雅满苏铁矿地球化学特征及矿床成因[J].西北地质,1995(1):15-19.
[14]张江,张相周.新疆哈密雅满苏铁矿床地质,地球化学特征及成因探讨[J].冶金地质动态,1995(12):9-11.
[15]肖滋泽.新疆雅满苏地区高光谱遥感地质解译及找矿预测研究[D].昆明:昆明理工大学,2015.
[16]蒋睿卿,冯友全.新疆鄯善县帕尔岗铁矿地质特征及成因分析[J].新疆钢铁,2014(4):49-53.
[17]王兴保.雅满苏铁矿床地质特征及成因浅析[J].地质找矿论丛,2005,20(b08):125-128.
[18]李万茂,陈国英,孙淑荣.新疆雅满苏铁矿床矿物共生组合的研究[J].大自然探索,1986(2):23-26.
[19]黎广荣,吴昌志.矽卡岩成因模式研究进展:兼论新疆雅满苏铁矿的成因[J].高校地质学报,2013(3):425-436.
[20]杨继兵,张克川,孙春霞.新疆哈密市雅满苏东北滩铜金矿地质特征及找矿方向[J].科技视界,2012(4):116-118.