共查询到20条相似文献，搜索用时 140 毫秒
1.
从理论上说,地球化学场与磁异常场的恒定关系是不存在的。但一个区域的地球化学特征与磁异常必然存在一定的关系,这种关系可能不是固定的。通过实际工作数据分析,证明了磁异常与地球化学异常确实有一定的关系,而且使用分频的磁异常研究与地球化学异常的关系会得到更合理的解释。分析的地球化学元素不同,与不同的频率磁异常会有不同的相关关系。 相似文献
2.
应用分形方法研究了新南威尔士地区地球化学异常及其下限的确定,对该区的地球化学铜元素异常区进行了圈定。通过与传统方法圈出的异常区进行比较,分形方法确定的异常下限更符合实际情况,并认为研究区域的东北部与南部存在铜矿床的可能性较大,为进一步找矿指明了方向。该方法不仅适用于地球化学铜元素数据,而且还适用于其他元素和地质数据,具有普遍的意义。 相似文献
3.
应用分形方法研究了新南威尔士地区地球化学异常及其下限的确定,对该区的地球化学铜元素异常区进行了圈定.通过与传统方法圈出的异常区进行比较,分形方法确定的异常下限更符合实际情况,并认为研究区域的东北部与南部存在铜矿床的可能性较大,为进一步找矿指明了方向.该方法不仅适用于地球化学铜元素数据,而且还适用于其他元素和地质数据,具有普遍的意义. 相似文献
4.
5.
6.
7.
地球化学模式及成因初探 总被引：4，自引：4，他引：4
如何对已发现的地球化学异常进行解释与评价，一直是困扰勘查地球化学家的难题。针对这一难题，笔者提出了地球化学模式的3种分类方案：规模分类、成因分类和成熟度分类。按照规模大小将地球化学模式分为：局部异常、区域异常、地球化学省、地球化学巨省和地球化学域， 同时将规模达地球化学省以上，并且内部具有套合结构特点的立体地球化学模式称作地球化学块体。地球化学模式依成因可分为原生地球化学模式和次生地球化学模式。成熟度分类是笔者首次提出，地球化学模式的成熟度是指地球化学异常相对于矿的关系而言的。笔者将地球化学模式按成熟度的不同，依次分为原始地球化学模式，中间地球化学模式和终极地球化学模式。提出成熟度分类是试图为科学利用所发现的地球化学模式进行异常解释与评价提供理论依据。 相似文献
8.
对新疆-甘肃-内蒙古衔接区的1：20万地球化学数据研究结果表明,该区Cu地球化学异常主要与基性、超基性岩和斑岩体有关,成矿元素组合为Co-Zn-Cr—Ni—Cu;W地球化学异常主要与中酸性岩有关,成矿元素组合为W—Sn—Bi。区内主要铜、钨矿床和新发现的矿床（点）均有相应元素区域异常显示,表明地球化学异常在本区具有重要指示意义。在全区确定了4个Cu地球化学省、5个W地球化学省、15个Cu区域异常和17个W区域异常,其中上马崖一铜山Cu地球化学省、黄山-梧桐窝子-葫芦北Cu地球化学异常带、土屋-赤湖Cu区域异常、大狐狸山Cu地球化学省、鹰嘴红山W地球化学省、古堡泉-柳园W地球化学省、英姿山W区域异常具有重要的找矿意义。 相似文献
9.
当地球化学数据并不服从正态分布或对数正态分布,甚至连数据转换之后也不服从正态分布时,很难用传统的方法进行统计分析。这里以一个具体的地区为例,应用了基于稳健统计学和EDA技术的地球化学异常下限确定方法,其具有简单和"稳健"的特点,也不要求数据服从任何分布。通过比较分析了基于稳健统计学和EDA技术的地球化学异常下限确定方法与传统方法的优缺点。实践表明,用该方法圈定的地球化学异常符合客观实际,异常范围大,与已知矿床(点)吻合很好。 相似文献
10.
对新疆—甘肃—内蒙古衔接区的1∶20万地球化学数据研究结果表明,该区Cu地球化学异常主要与基性、超基性岩和斑岩体有关,成矿元素组合为Co-Zn-Cr-Ni-Cu;W地球化学异常主要与中酸性岩有关,成矿元素组合为W-Sn-Bi。区内主要铜、钨矿床和新发现的矿床（点）均有相应元素区域异常显示,表明地球化学异常在本区具有重要指示意义。在全区确定了4个Cu地球化学省、5个W地球化学省、15个Cu区域异常和17个W区域异常,其中上马崖—铜山Cu地球化学省、黄山—梧桐窝子—葫芦北Cu地球化学异常带、土屋—赤湖Cu区域异常、大狐狸山Cu地球化学省、鹰嘴红山W地球化学省、古堡泉—柳园W地球化学省、英姿山W区域异常具有重要的找矿意义。 相似文献
11.
Panfeng Liu Xianrong Luo Meilan Wen Jiali Zhang Wen Gao Fei Ouyang Xuchuan Duan 《中国地球化学学报》2018,37(3):402-413
Exploration for buried gold ores and other deeply buried ores, especially in high altitude localities, is one of the tough challenges facing the geological world today. Fast and efficient ore prospecting methods are badly needed to deal with the situation. This paper documents a test that, for the first time, uses an electrogeochemical approach to prospect ores in the alpine meadow-covered Bangzhuoma area and its periphery in Qinghai–Tibet Plateau. The results were compared with conventional soil measurements from a 2D prospection, and an ideal model of electrogeochemical anomaly formation in the area was established based on the comparison in order to provide theoretical guidance to buried ore prospecting in areas with similar conditions. The research shows that: (1) For exploration of deeply-buried mineral deposits, an electrogeochemical approach is better than soil measurements in terms of correspondence between element content values and anomaly forms and spatial distribution of known deposits in sections. Anomalies of high to low temperature element associations (Bi–Mo; Au–Ag–As–Bi and Au–Ag) and clear zonation were also observed along vertical vein runs in the sections. Based on integration of the observation with geological characteristics of the sections, we propose to use Au, Ag and As as the electrogeochemical indicators and Bi and Mo as the electrogeochemical tracing elements to guide further analysis. (2) Judging from element statistics and the scale, intensity, and range of anomalies in plan maps, we found that an electrogeochemical approach is less affected by topography and secondary actions. The plan maps also show that elemental differentiation coefficients of the study area are in an ascending order of Ag (0.67) < Mo (0.85) < Bi (0.97) < Au (1.51) < As (2.35), better representing the element distribution in the area and yielding more striking and concentrated anomalies for known deposits than that of the soil measurements. Apart from that, electrogeochemical anomalies were observed in the south of lines 002 and 003 and the central of lines 008 and 009. We suggest the existence of deeply-buried mineral deposits based on analyses of element combinations and gold grade variations in samples taken from exploratory trenches in the area. (3) A three-stage (referring to the ore body dissolution, the mineralogenetic particle migration, and the mineralogenetic particle unloading) electrogeochemical ideal model was established for the study area, which takes into account moderate rainfall, high altitude, low air pressure, well-developed vegetation and roots, and an Upper Triassic Nieru Formation carbonaceous sandy slate as overburden. 相似文献
12.
A new electrogeochemical extraction technique has been used in cooperation with the field paper chromatographic method to determine gold which migrates in ionic form and is deposited on the electrode inserted in the soil. The technique has been tested with encouraging results in several Au areas. The results indicate that distinct Au anomalies can be discovered which have been buried by transported overburden. 相似文献
13.
14.
15.
The problem of using surface geochemical exploration techniques in areas of very thick and electrically conductive weathering residuum is common to much of Australia. At the Elura deposit (New South Wales) a distinct electrogeochemical H+ anomaly can be detected in the top few cm of residual soil above about 100 m of conductive residual overburden. In the present paper the results of an investigation of the much more difficult problem of detecting sulfide mineralization beneath thick conductive transported overburden are described.The objective of the study was to demonstrate that sulfide mineralization beneath thick transported overburden can be detected by geochemical patterns in surface soils in the context of an electrogeochemical model of dispersion.The Thalanga massive sulfide deposit in northeast Queensland has at least 4 million tonnes of 15% combined Zn, Pb and Cu. The mineralized horizon lies at the contact between rhyolitic and dacitic rocks of the Cambro-Ordovician Mt. Windsor Volcanics. The deposit is covered by transported cemented Tertiary terrigenous clayey sandstones and grits; these are electrically conductive and vary in thickness from 0 to 70 m.Near-surface soil samples were collected along five traverses normal to the strike of mineralization. The traverses were located to give 0 m, 1 m, 30 m, 50 m, and 70 m overburden thicknesses; there is no known significant mineralization along the last traverse which is assumed to be background, and there is a small gossan where the overburden is absent.Dispersion patterns influenced by electrogeochemical processes should result in relatively low values for ions over massive sulfides with lateral peaks; this has been termed a “rabbit-ear” anomaly. “Rabbit-ear” anomalies in surface soils for H+, Cu, and Zn occur over the sulfide zone. The H+ pattern is better defined where there is a significant depth of overburden (where the anomaly is about 500 m wide). The Cu anomaly is 300–600 m wide, and the Zn anomaly is 450–675 m wide.Even where the overburden is 50 m thick, anomalous “rabbit-ear” anomalies for H+ and Zn are clearly identifiable, but the anomaly for Cu is a single peak of 20 ppm over the hanging wall. It is suggested that the results of this work convincingly demonstrate that at Thalanga surface soil samples may reliably be used to detect massive sulfide deposits - even where they are effectively blind beneath a considerable thickness of transported and conductive overburden. The processes of dispersion are speculated to be diffusion, and it is argued that the pattern-controlling mechanism is electrochemical. 相似文献
16.
金属矿床地电化学勘查方法研究现状及前景展望 总被引：6，自引：0，他引：6
地电化学勘查方法是20世纪70年代兴起的找寻隐伏矿床的新方法之一,包括地电提取法和土壤离子电导率测量法。它从20世纪70年代到90年代末这30多年的发展中一直被地学专家列为新的前缘课题来研究,它所提取的成矿信息来自于深部矿体,这一点经国内外科研工作者多年的找矿实践所证实,毋庸质疑。由于前苏联研制的“部分提取金属法”设备笨重、野外工作效率低、成本高而一直未能得到普及应用,随着方法技术的不断改进,其适用范围有所扩展,为地电化学方法找寻隐伏矿床开拓了广阔的道路。 相似文献
17.
深穿透地球化学对比研究两例 总被引：13，自引：0，他引：13
为了寻找隐伏矿床,近些年提出了深穿透地球化学的概念和发展了深穿透地球化学方法。国际勘查地球化学家协会于1997年开始组织实施了“深穿透地球化学对比计划”。这里给出了四种深穿透地球化学方法,包括金属活动态提取方法、酶提取方法、活动金属离子法和电地球化学方法,在中国和美国的两个隐伏矿进行了对比试验,结果表明,深穿透地球化学方法可以在隐伏矿上方有效地发现异常。在干旱荒漠区,由于氧化作用和蒸发作用强烈,地表形成氧化地球化学障和大量盐类的蒸发地球化学障,这些地球化学障可以将深部迁移至地表的含矿信息捕获。因此,用深穿透地球化学的铁锰氧化物膜提取和盐类蒸发障良好导电性能的电提取,可以有效地指示矿体。中国的深穿透地球化学方法在美国内华达Mike金铜矿的效果要优于加拿大的酶提取(EnzymeLeach)和澳大利亚的活动金属离子法(MMI)。 相似文献
18.
通常运用地质、地球物理以及钻探的方法来确定金属矿体的赋存状态,地球物理方法中常用的探测手段主要有地面伽玛能谱测量法、X射线荧光法、浅层地震、地电化学参数法和地电化学提取法等.SYT法接收反射回来的带有地下地质信息的电磁波,再经过特殊的数据处理而得到的反映地下地层物性特征的曲线和柱状,可以用来进行地质解释,运用该方法对山东牟平隐伏区的含金矿化异常带进行了探测研究,探测结果显示,在SYT法探测曲线中,含金矿化带有明显的异常特征,可以用来确定金属矿体的埋深和厚度. 相似文献
19.
Yu. O. Gavrilov 《Lithology and Mineral Resources》2010,45(2):120-135
Migration and accumulation of sulfides at the contact of lithologically and geochemically different layers are considered.
The possible mechanisms (gravitational, diffusion, elision, and electrogeochemical) for sulfide transportation during diagenesis
are discussed. Data are presented to explain the localization of sulfide minerals at the boundary of reduced and oxidized
sediments. The paper considers examples of stratiform sulfide concentrations of not only ore grade, but also lower grade,
which, however, are of great significance for understanding the formation conditions of some geochemical anomalies. Link between
the diagenetic migration of sulfides and the formation of iridium anomaly is substantiated. 相似文献