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1.
杏山北钼矿床为胶东半岛一典型矽卡岩型钼矿床,位于著名牟平乳山金成矿带和蓬莱栖霞金成矿带之间,区域上位于胶东辽东钼成矿带,具有较好的成矿地质条件。通过对比胶东地区其他典型钼矿床地质特征,认为胶东半岛钼矿床存在两期成矿时代;矽卡岩型矿床主要受近EW向断裂构造控制,斑岩型矿床主要受近EW向与NE向断裂复合构造控制。通过物探异常预测,认为杏山北钼矿床深部是寻找矽卡岩型和斑岩型铜钼矿床的有利部位。  相似文献   

2.
西准噶尔成矿带是中亚成矿域巴尔喀什成矿带的东延部分,目前已发现有包古图斑岩型铜矿床、哈图金矿床、萨尔托海铬铁矿床和杨庄铍矿床等大型超大型矿床,是中亚成矿域内重要的成矿远景区.北东向达拉布特断裂、玛依勒断裂、巴尔鲁克断裂等以及所夹的构造地块,构成了西准噶尔“多”字型构造体系(简称“西准系”),是控制西准噶尔成矿带铜-金-...  相似文献   

3.
中国北部得尔布干成矿带构造演化与成矿作用   总被引:8,自引:0,他引:8  
得尔布干断裂带控制了火山 侵入杂岩作用 ,形成了多金属成矿带。多期次构造 岩浆活动 ,在成矿带内形成了不同时期规模不等的侵入岩体及大面积分布的中生代火山岩。在区内已发现金、银、铜等多金属矿产地百余处 ,矿床空间分布明显受断裂控制。研究表明 :得尔布干断裂带经历了加里东期到第三纪多期构造演化并伴有相应的岩浆活动。深断裂控制区域构造发展 ,次级断裂对成矿起导矿、容矿作用。本文从构造控矿作用入手 ,分析研究区内各类矿床的构造控矿因素 ,提出了成矿带内多级构造控矿作用 ,对今后在我国东北部找矿有一定的指导意义。  相似文献   

4.
西南“三江”成矿带北段区域成矿断裂信息定量化分析   总被引:3,自引:1,他引:2  
董庆吉  肖克炎  陈建平  丛源 《地质通报》2010,29(10):1479-1485
"三江"北段成矿带是中国著名的"三江"铜多金属巨型成矿带的北延部分,构造上属特提斯巨型成矿域的重要组成部分,区域成矿条件极为优越。区内矿床主要为斑岩型铜钼矿床和热液型铅锌矿床,成矿主要受断裂构造的控制,定量分析成矿断裂信息对于指明区域找矿方向至关重要。以GIS技术为平台,采用断裂等密度、断裂中心对称度、断裂优益度、断裂交点数、断裂频数等参数定量地分析区域断裂信息,从中提取区域主干断裂发育区和次级断裂发育区。区域成矿特征表明,本区矿床沿区域主干断裂成带状分布,而次级断裂发育区为主要的矿床赋存区。通过定量分析发现,本区2个主要矿集区之间的扎青乡地区存在一个成矿断裂信息异常高值区,认为是本区今后找矿的有利区域。  相似文献   

5.
湘南多金属矿集区是一个世界级的多金属矿集区,包含有三条有色多金属亚成矿带。其成矿活动与深大断裂带关系密切,深大断裂为深部成矿物质提供了构造通道条件,控制了矿集区内多金属亚成矿带的形成和分布,深大断裂的交汇部位则控制了大型、超大型矿床(田)的产出。  相似文献   

6.
河北丰宁营房-牛圈银矿床构造控矿特征和成因探讨   总被引:14,自引:3,他引:11  
魏晓英 《地质找矿论丛》2000,15(3):261-266,281
研究了营房-牛圈矿床成矿物质基础,来源、分析构造控矿特征;认为深大断裂控制岩尔成矿带,线环交织构造控制流体,流切带控制矿空间位置;提出银矿宋属深源热流体隐暴-交代型矿床。  相似文献   

7.
智利阿塔卡玛断裂(AFZ)走滑扩张构造与控矿作用   总被引:2,自引:0,他引:2  
智利北中部安第斯海岸山系发育大量的铁铜金及贵金属矿床,构成了阿塔卡玛断裂(Atacama Fault Zone,AFZ)成矿带,是重要的富含铁氧化物成矿带.中生代板块的俯冲消减导制多期次岩浆弧的演化和衰退,形成了目前主体南北向构造格架并控制了金属成矿带的分布.  相似文献   

8.
安徽省庐江县沙溪铜矿床地质特征及形成时代   总被引:1,自引:0,他引:1  
长江中下游成矿带是中国东部重要的多金属成矿带之一。安徽省庐江县沙溪铜矿床位于长江中下游成矿带中部,是该成矿带内目前发现的规模最大的斑岩型铜矿床,勘探工作表明矿床的深部和外围有良好的找矿前景。1矿区地质特征沙溪铜矿床位于滁州-庐江构造岩浆带的西南部,产于郯庐断裂的主干断裂带内,距庐枞火  相似文献   

9.
郭玲利 《安徽地质》2016,26(3):194-197
研究区金矿床位于胶莱盆地东北缘,牟乳成矿带西侧,是郯庐断裂带重要分支-郭城断裂带内的主要矿床之一,其矿体严格受NNE和NEE向次级压扭性断裂控制。本文对研究区矿床成矿物质来源、矿床成因模式等特征进行了研究,简要的总结了其成矿过程。  相似文献   

10.
三家子金矿位于冀东金成矿带东部,矿区内分布大量受断裂构造控制的含金石英脉,通过野外和室内研究,确定其成矿物质来源于燕山期岩浆期后热液。这些成矿热液在沿矿区内深大断裂F1向上运移过程中,部分成矿物质在F1断裂沿走向变化处发生沉淀,其它成矿物质在F1断裂派生的次级张裂隙中沉淀。该矿床属于受断裂控制的中低温、岩浆期后热液矿床。  相似文献   

11.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

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14.
正1 Introduction Geological studies established on several sections in Lanping-Simao basin have shown that the salt-bearing strata of Mengyejing formation(Yunlong Fm.in Lanping basin)are constituted by an alternation of salt layers and interbedded facies.The latter consists mainly of mudstones,and mudstone-rich conglomerate.The mineralogy and geochemistry of salt-bearing beds and  相似文献   

15.
正On 22nd April 2014,with the approach of the 45th World Earth Day,China’s Ministry of Land and resources issued the status of China’s mineral resources in 2013.The first task of the prospecting breakthrough strategy action implemented in the last five years has been completed,and China’s security capacity for mineral resources has been significantly improved.In the  相似文献   

16.
正There are more than 700 salt lakes with area of more than 1km2 on the Qinghai-Tibet Plateau of China.In recent years,an oilfield brine was also found in the Nanyishan Section of Qaidam Basin in the Qinghai-Tibet  相似文献   

17.
正1 Introduction Physical and numerical models are constructed to investigate the evolution and mechanism of salt migration driven by tectonic processes.In recent years,we have designed and ran series of models to simulate salt  相似文献   

18.
正The study of Cretaceous-Palaeogene salt-bearing strata of the Khorat Basin Laos and the Lanping-Simao Basin in Yunnan,China has an great significance not only in explaining the basin evolution and the genesis of potash  相似文献   

19.
正Potash is one of the long-term scare deposits in China,and potash prospecting has long been listed as a key brainstorm project for our nation and geological prospecting units.There have been considerable studies in search for potash deposits in the Kuqa depression of the Tarim basin(Jackson et al.,1991;Gemmer et al.,2004;Vendeville,2005;Vendeville and Jackson,1992a,1992b),  相似文献   

20.
正1 Introduction Qaidam Basin in Qinghai,including 43 salt lakes with multiple dominant mineral such as potassium,magnesium,lithium etc.,is the most intensive distribution of Saline  相似文献   

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