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1.
贵州织金县新华磷矿大戛矿段矿床特征及成矿   总被引:1,自引:0,他引:1  
阐述了织金县新华磷矿大戛矿段地质背景和特征,在对区域地质的研究基础上,通过对矿体形态特征、矿石结构构造、成分分析,总结出该地区成矿条件,矿体往深部还有较大延伸空间,矿床深部具有较大的资源远景。  相似文献   

2.
庙山金矿位于秦岭造山带西秦岭中部花岗岩带,属北中秦岭陆表海盆中段。赋存于高桥—洮坪大断裂西段。通过对金矿体地质及矿带特征较为客观认识的基础上,分析总结矿体控矿因素指导深部探矿。经深部坑探,矿体氧化深度较深(最深178m),矿体向深部有变富变厚的趋势。庙山金矿属断裂破碎带控制的中低温热液蚀变岩型金矿。  相似文献   

3.
为预测范庄银矿床M_(23)主矿体的深部变化趋势,在对矿区地质特征和矿床成因研究的基础上,开展了野外地质调查及地球化学研究。结果发现矿体具有明显的侧伏现象。微量元素统计分析表明,Cu、Sb、As为矿体的近矿指示元素,矿体具有多期次的特点。M_(23)矿体化探数据表明,矿体自上而下其原生晕轴向分带序列为:Au-Bi-Cu-As-Zn-Pb-Sb-Mo-Ag-Sn-W-Hg,具有明显的"头尾晕共存"和"反分带"特征。结合矿体剥蚀系数的变化规律,预测在M_(23)矿体向深部(696 m以下)有较大延深(伸)或有深部有盲矿体存在,钻探验证(见矿高程370 m)说明矿床深部有较大的增储潜力。  相似文献   

4.
河南省石盘沟金矿构造控矿特征研究   总被引:1,自引:0,他引:1  
区内矿体受拆离断层的控制而沿拆离断层分布 ,空间定位在其两侧 15 0~ 6 0 0 m的垂直距离内 ;NE- NNE向含金破碎带是金矿的主要容矿构造 ,其走向向 NNE偏转地段和陡倾斜处是矿体富集的有利部位 ;矿床在成矿后受到枯桩杈断裂的破坏 ,使其南北两侧矿体的地质特征有较大差异 ,北侧剥蚀严重 ,南侧深部找矿前景良好  相似文献   

5.
广东韶关凡口铅锌矿狮岭南区段的开拓工程已延伸至-550m中段,矿体呈现尖灭趋势。为查明深部区域地层矿化特征、构造控矿特点,并指导深部寻找盲矿体,通过收集分析中上部各中段地质资料,并与地质勘查资料对比,利用坑道设计并施工了9个孔深300 m左右的坑内探矿钻孔,进一步查明了狮岭南深部地质特征,并在F3断裂下盘探获多条盲矿体。F3断裂既是导矿构造,也是重要控矿构造,其下盘至F203断裂之间的夹持带为狮岭南深部有利成矿空间  相似文献   

6.
马思罗金矿赋存于中三叠统盐塘组浅海相含火山喷发物的不纯碳酸盐岩中,金矿化受岩性控制。笔者通过对马思罗金矿床的地质特征、控矿因素及矿床成因的系统研究,总结了找矿标志,分析了找矿前景。认为矿区内化探综合异常有待于查证,有望发现新矿体;已知矿体的两侧及深部有待于控制,有望扩大矿区规模,矿区仍有较大的找矿远景  相似文献   

7.
莱州寺庄金矿床深部地质特征   总被引:3,自引:0,他引:3  
山东省第六地质矿产勘查院通过对山东省焦家断裂金矿带近5年的深部地质找矿工作,在该带南部地段的寺庄金矿床的深部发现了特大型破碎带蚀变岩型金矿.该深部金矿床与产于第一矿化富集带中的浅部金矿床之间有100~250 m垂深的无矿间隔,构成第二矿化富集带.通过深部勘查,寺庄金矿床深部范围内共圈出Ⅰ、Ⅱ、Ⅲ号3个矿体群、163个矿体.其中,在主裂面下盘的黄铁绢英岩化碎裂岩带内发现了规模较大盲矿体Ⅰ-1号矿体,其资源储量占总量的39.39%,取得了深部找矿的重大突破.笔者从寺庄矿区地质特征、寺庄金矿床深部地质特征等方面进行了论述.对同类型矿床的深部找矿工作具有重要的理论和实践意义.  相似文献   

8.
刘屯金矿床由刘屯(Ⅰ)和金屯(Ⅱ)两个地段组成.作者通过矿床地质特征、深部地球物理特征、金矿体地球化学异常模式判别及矿体剥蚀程度预测等研究,对刘屯金矿床深部成矿提出了新看法,认为Ⅰ地段矿体已剥蚀到中下部,40 m以下矿化尖灭;Ⅱ地段矿体剥蚀至头部,向下有较大延深,可进一步开展深部找矿.  相似文献   

9.
山东省文登市西院下金矿成矿规律及深部矿体定位预测   总被引:2,自引:1,他引:1  
在地质工作的基础上,运用计算方法,深入剖析西院下金矿床的地质特征,总结控矿和成矿规律,对金矿深部进行了矿体定位预测,指出探矿方向,并设计了相应的验证工程。  相似文献   

10.
詹德光 《地质与勘探》2015,51(3):478-485
安徽铜山铜矿已有近50年的开发历史。为建立具有预测能力的新成矿模式,本文对该矿床的地质背景、矿体地质特征、控矿构造以及矿体定位空间的分布规律和形成机制进行了深入研究。研究认为,矿体受与接触带套合的波状起伏的伸展断层控制,矿体的位置及规模受接触带断层的不均匀扩容制约。基于这些认识,建立了波状接触带-断层伸展剪切扩容构造控矿理论模式并根据这一理论模式预测矿床的深部存在大规模隐伏矿体。钻探结果证实了这一预测结论,表明新的成矿理论模式将在铜山的深部找矿勘查中发挥重要作用。  相似文献   

11.
International unity is becoming ever stronger in this country owing to an increasing similarity in the development of the cultural environment. This comprises the provision of all the country's republics with a sufficient number of schools, theatres, and other institutions and cultural information media in accordance with the needs of the population. An important part is played by the rise in ‘the general educational level, as well as the level of professional qualifications and skills. Among all the Soviet nations and nationalities, this rise being more rapid among formerly backward peoples. Prominent among the factors of internationalization is the progressive development of the nationalities’ cultural resources, while professional culture is being increasingly brought within the reach of the masses.The implementation of the nationalities policy promotes the all-round development of all Soviet nations and nationalities, their drawing together, the upsurge of the individual capabilities of every Soviet citizen.  相似文献   

12.
The Global Stratotype Section and Point (GSSP) for the base of the Silurian System was defined in 1985. Since that time, a number of researchers have suggested that this section has serious deficiencies for use as a GSSP. As a result, in 2000, the Subcommission on Silurian Stratigraphy (SSS) proposed undertaking a formal restu@ of this GSSP, which was subsequently approved by the International Commission of Stratigraphy (ICS). The result of this restudy was the formal proposal that the current GSSP, at 1.6 m above the base of the Birkhill Shale, at Dob's Linn, Scotland, should be maintained as the same locality and stratigraphic level, but the bios- tratigraphical definition of the boundary should be revised. The previously defined, basal Silurian grapto- lite zone, the Parakidograptus acuminatus Zone, should be subdivided into a lower Akidograptus ascensus Zone and a higher E acuminatus Zone. The base of the A. ascensus Zone, marked by the first appearance of A. ascensus, should be regarded as the biostratigraphic mark for the base of the Silurian. This proposal has now been formally approved by the SSS and ICS, and ratified by International Union of Geological Sciences. This is the first GSSP to undergo formal restudy and redefini- tion, and the proposal also included a recommended procedure for restudy of GSSPs.  相似文献   

13.
It is known from observations that the center of mass of the Moon does not coincide with the geometric center of its figure, and the line connecting these two centers is not aligned with the direction toward the center of the Earth, instead deviating toward the Southeast. This stationary deviation of the axis of the inertia ellipsoid of the Moon to the South of the direction toward the Earth is analyzed. A system of five linear differential equations describing the physical libration of the Moon in latitude is considered, and these equations are derived using a new vector method taking into account perturbations from the Earth and partly from the Sun. The characteristic equation of this system is obtained, and all five oscillation frequencies are found. Special attention is paid to the fifth (zero) frequency, for which the solution of the latitude libration equations are stationary and represents a previously unknown additional motion of the rotational axis of theMoon in a cone with a small opening angle. In contrast to the astronomical precession of the Earth, the rotation of the angular-velocity vector is in the positive direction (counter-clockwise), with the period T 3 = 27.32 days. On this basis, this phenomenon has been named “quasi-precession.” This quasi-precession leads to a stationary inclination of the major axis of the inertia ellipsoid of theMoon to the South (for an observer on Earth), making it possible to explain one component of the observed deviation of the center of mass of the Moon from the direction toward the Earth. The opening angle of the quasiprecession cone is approximately 0.834″.  相似文献   

14.
Important tendencies in development of the world mineral-resources sector at the beginning of the 21st century were an increase in production and consumption of mineral materials differentiated by types of metals and nonmetallic mineral raw materials, by countries and regions, as well as the concentration of the production of mineral raw materials in a small number of countries, and a reduction in industrial reserves of minerals in the world economy, even at the current stage of their extraction. These tendencies should be taken into account in working out a strategy for development of the Russian mineral raw-material base.  相似文献   

15.
Taking the example of W Sudan, an analysis of the climatic incidents leading to the two recent famine disasters is made. On this natural background, the human side is investigated. Focus is directed towards the fragile economic structure of the famine-prone population groups. An early-warning system for famine in the Sahelian Zone is proposed taking grain production and storage, livestock development and the relationship between the prices of livestock and grain as major indicators.  相似文献   

16.
东濮凹陷北部沙三中亚段广泛发育盐岩和烃源岩,这两个看似不能共存的物质却在这里互层共生。该时期研究区沉积特征为多盐韵律与多层烃源岩互层共生、连续沉积,单个盐韵律厚度从几米到十几米,烃源岩有机质丰度高、类型好。平面上,两者在湖盆沉积沉降中心共生;垂向上,高有机质丰度、好干酪根类型与高盐度地层具有较好的对应关系。因而成为恢复古气候和古环境的重要研究对象。通过岩石学、古生物学以及Sr/Ba、B/Ga、(V+Ni+Mn)、Fe/Mn、Sr/Cu、Mg/Ca、V/(V+Ni)、稀土元素含量和氯同位素等方法对凹陷北部沙三中亚段的沉积环境进行研究。结果表明,凹陷北部沙三中亚段为深水沉积的还原环境,古盐度较高,达到半咸水-咸水沉积;微量元素和孢粉化石特征表明研究区沙三中亚段为温暖潮湿的环境。  相似文献   

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19.
郯庐断裂南段研究进展与断裂性质讨论   总被引:13,自引:3,他引:13  
据1:5万区域地质调查和专题研究资料,就郯庐断裂带是否南延与消失的原因,其与大别—苏鲁造山带交截形成的假位错效应,以及与中新生代沉积盆地形成演化的关系等作了新的阐述。在此基础上,讨论了郯庐断裂带是否为巨大的左行平移断层或转换断层。认为郯庐断裂带可能是在“古郯庐带”的基础上于早侏罗世重新活动、白垩纪强烈活动的地堑型枢纽断裂带。  相似文献   

20.
In order to characterise the influence of the heavyrains on the observed landslides during the 1996–1997hydrological cycle, rainfall records for the last 100years are analysed from 104 stations in easternAndalusia. Regarding the amounts of rain recordedbetween October 1996 and March 1997 in the 104stations studied, 31 presented new all-time records;15 presented values that were 80–100% of thepre-1995 record; 49 stations, 80–50%; and 9stations, < 50%. A map has been devised of thesusceptibility of the materials through which thesouth-eastern Andalusian road network crosses,together with an inventory of the damage caused byinstability phenomena on banks and cuttings of theroad network during the winter of 1996–1997. Therelationships between the rainfall during the studyperiod, the damage caused to the road network and thesusceptibility of the materials affected are analysed.The results indicate that there is a clearcorrespondence between the rainfall recorded and thesusceptibility of the materials with the inventorieddamage. It is concluded that the widespread seriousdamage caused in early 1997 to the roads andsurrounding areas in the Alpujarra region and thecoast of the Province of Granada was mainly caused bythe extraordinarily heavy rains. However, considerablyless damage was observed where the susceptibility ofthe terrain is low, thus highlighting the extremeusefulness of terrain-susceptibility maps for riskprevention and territorial planning.  相似文献   

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