CN116165708A - Accurate positioning method for uranium-bearing ore-forming sand body with beneficial coverage area - Google Patents
Accurate positioning method for uranium-bearing ore-forming sand body with beneficial coverage area Download PDFInfo
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Abstract
Description
技术领域technical field
本发明属于铀成矿有利砂体预测技术领域,具体涉及一种覆盖区有利铀成矿砂体的精确定位方法。The invention belongs to the technical field of prediction of favorable uranium ore-forming sand bodies, and in particular relates to a precise positioning method for favorable uranium ore-forming sand bodies in coverage areas.
背景技术Background technique
砂岩型铀矿是我国重要的工业铀矿化类型,随着节能减排、环保绿色理念的提出,提供经济可采铀矿资源来满足我国军工、核电发展至关重要。砂岩型铀矿因其埋深浅,易开采、安全环保的特点而迎来全面快速发展阶段。上世纪九十年代起至今,我国分别在鄂尔多斯、二连、松辽、伊犁等盆地取得了较大突破,落实了皂火壕、纳岭沟、大营、钱家店、蒙其古尔等特大型铀矿床,形成了一系列找矿方法,极大地丰富了我国砂岩型铀资源储量。Sandstone-type uranium ore is an important type of industrial uranium mineralization in my country. With the concept of energy saving, emission reduction and environmental protection, it is very important to provide economically recoverable uranium resources to meet the development of my country's military industry and nuclear power. Sandstone-type uranium mines have ushered in a comprehensive and rapid development stage due to their shallow burial depth, easy mining, safety and environmental protection. Since the 1990s, my country has made great breakthroughs in the Ordos, Erlian, Songliao, and Yili basins, and implemented the Zaohuohao, Nalinggou, Daying, Qianjiadian, Mengqigul and other basins. The extra-large uranium deposits have formed a series of prospecting methods, which have greatly enriched the reserves of sandstone-type uranium resources in my country.
近年来,随着砂岩型铀矿勘探程度的不断加深,逐渐认识到砂岩型铀矿成矿机理多为复合成因,但是有利成矿砂体的定位预测技术仍是找矿的关键技术,因此,需要设计一种覆盖区有利成矿砂体精确定位技术方法,用于完善现有成矿砂体定位预测工作中,预测准度欠佳的技术问题。In recent years, with the continuous deepening of the exploration of sandstone-type uranium deposits, it is gradually recognized that the ore-forming mechanism of sandstone-type uranium deposits is mostly of composite origin, but the location prediction technology of favorable ore-forming sand bodies is still the key technology for ore prospecting. Therefore, it is necessary to A technical method for precise positioning of favorable ore-forming sand bodies in the coverage area is designed to improve the technical problems of poor prediction accuracy in the existing positioning and prediction of ore-forming sand bodies.
发明内容Contents of the invention
本发明设计的一种覆盖区有利铀成矿砂体的精确定位方法,用于解决现有成矿砂体定位预测工作中由于铀矿成矿机理复合成因多,易导致定位准度欠佳的技术问题。An accurate positioning method for favorable uranium ore-forming sand bodies in the coverage area designed by the present invention is used to solve the technical problem of poor positioning accuracy due to multiple uranium ore-forming mechanisms and multiple causes in the existing ore-forming sand body positioning and prediction work .
本发明的技术方案:Technical scheme of the present invention:
一种覆盖区有利铀成矿砂体的精确定位方法,包括如下步骤:A method for precisely locating favorable uranium ore-forming sand bodies in an overlay area, comprising the following steps:
步骤1、收集、分析资料,圈定具有较大潜力重点找矿盆段、地区;Step 1. Collect and analyze data, delineate key prospecting basins and areas with great potential;
步骤1.1、初步圈定重点盆段;Step 1.1. Preliminary delineation of key basin segments;
步骤1.2、在步骤1.1圈定的重点找矿盆段基础上,圈定重点地区;Step 1.2, on the basis of the key prospecting basin sections delineated in step 1.1, delineate key areas;
步骤2、厘定有利找矿目标层位;Step 2. Determine the favorable prospecting target layer;
步骤3、补充收集钻穿步骤2中厘定的有利找矿目标层位的钻孔资料,统计目标层位各类控矿要素的数据;Step 3. Supplementary collection of drilling data for drilling through the favorable ore prospecting target layer determined in step 2, and statistics of data on various ore-controlling elements of the target layer;
步骤4、利用Surfer软件绘制目标层位各控矿要素图件,筛选各要素最有利成矿区间;Step 4, use Surfer software to draw the map of each ore-controlling element in the target layer, and screen the most favorable mineralization interval of each element;
步骤5、对各类图件套合叠置,精确定位有利铀成矿砂体。Step 5. Overlap and overlay all kinds of maps to accurately locate favorable uranium ore-forming sand bodies.
所述步骤1.1、初步圈定重点盆段,包括:收集研究盆地的区域地质、大地构造演化等图文资料,明确盆地类型、沉积盖层、基底岩性、蚀源区条件等要素,按照一级构造单元圈定具有较大潜力重点找矿盆段:The step 1.1, preliminary delineation of key basin sections, includes: collecting graphic data such as regional geology and tectonic evolution of the research basin, clarifying elements such as basin type, sedimentary cover, basement lithology, erosion source area conditions, etc., according to the first-level Structural units delineate key prospecting basins with great potential:
所述挤压盆地类型一级构造单元以山前斜坡带、裂陷盆地类型一级构造单元以隆起区为首选;The first-order structural unit of the extrusion basin type is the piedmont slope belt, and the first-order structural unit of the rift basin type is the uplift area;
所述沉积盖层以发育层间氧化带且厚度<1000m为有利;It is favorable for the sedimentary cover layer to develop an interlayer oxidation zone with a thickness <1000m;
所述蚀源区岩性花岗岩为首选,火山碎屑岩、酸性火山岩次之,铀含量≥5ppm。Lithological granite in the erosion source area is the first choice, followed by pyroclastic rock and acidic volcanic rock, with uranium content ≥ 5ppm.
所述步骤1.2在步骤1.1圈定的重点找矿盆段基础上,圈定重点地区,包括:着重收集整理该盆段地质、构造、地震数据,研究分析该盆段沉积体系、古气候演化、物源—铀源供给条件等要素,划分二级构造单元并据此进一步圈定有利成矿重点地区:依据步骤1.1中有利沉积盖层厚度在垂向上界定有利成矿地质年代范围;整合前期现有研究资料、分析该盆段古气候、沉积演化特征,确定垂向上以半干旱—半潮湿气候条件、沉积体系以河流—三角洲体系为有利;综合上述有利要素,以二级构造单元为单位,横向上保证物源—铀源供给充足,以靠近物源区、蚀源区或构造剥蚀区为有利,进而综合研判圈定有利成矿重点地区。The step 1.2 delineates the key areas on the basis of the key prospecting basins delineated in step 1.1, including: focusing on collecting and sorting out the geological, structural, and seismic data of the basins, and researching and analyzing the sedimentary system, paleoclimate evolution, and provenance of the basins — Uranium source supply conditions and other factors, divide the secondary structural units and further delineate the key areas of favorable mineralization: according to the thickness of the favorable sedimentary cap rock in step 1.1, define the range of favorable mineralization geological age vertically; integrate the existing research data in the previous period 1. Analyze the paleoclimate and sedimentary evolution characteristics of this basin section, and determine that the semi-arid-semi-humid climate conditions in the vertical direction and the river-delta system in the sedimentary system are favorable; Provenance—uranium source is sufficient, and it is advantageous to be close to the provenance area, erosion source area or structural denudation area, and then comprehensively study and judge to delineate the key areas of favorable mineralization.
步骤2、厘定有利找矿目标层位包括:Step 2. Determining favorable prospecting target layers includes:
步骤2.1、在步骤1圈定的重点地区范围内,收集钻孔资料,所述收集钻孔资料覆盖全区的地震剖面等资料;Step 2.1, within the key areas delineated in step 1, collect borehole data, and the collected borehole data cover the seismic profiles and other data in the whole area;
步骤2.2、垂向上,利用钻孔数据资料建立多个典型单井柱状图,结合区域上的地震剖面等资料明确地层厚度,建立该重点地区综合柱状图;在此基础上对各地层间、层组内的岩性结构进行分析,结合前期现有研究成果优选垂向上有利岩性组合以发育稳定的泥-砂-泥结构为主的地层;Step 2.2, vertically, use the drilling data to establish multiple typical single-well histograms, combine the regional seismic profile and other data to clarify the stratum thickness, and establish a comprehensive histogram for this key area; Based on the analysis of the lithological structure within the formation, combined with the previous research results, the vertically favorable lithological combination is selected to develop a stable mud-sand-mud structure;
步骤2.3、横向上,绘制连井剖面,以层组为单位进一步划分沉积相带、砂体发育、层间氧化带等要素、确定以辫状河流相、曲流河河道亚相、辫状河三角洲相平原亚相;发育多层砂体且单层砂体厚度在5-15m,连续性较好;层间氧化带发育规模大的层位为有利目标层位。Step 2.3. Horizontally, draw the well-connected section, further divide the sedimentary facies belt, sand body development, interlayer oxidation zone and other elements in units of formations, and determine the braided fluvial facies, meandering river channel subfacies, and braided fluvial facies. Delta facies plain subfacies; multi-layer sand bodies are developed and the thickness of a single layer of sand bodies is 5-15m, with good continuity; the layers with large-scale development of interlayer oxidation zones are favorable target layers.
所述步骤3、补充收集钻穿步骤2中厘定的有利找矿目标层位的钻孔资料,统计目标层位各类控矿要素的数据;The step 3, supplementary collection of drilling data for drilling through the favorable ore prospecting target layer determined in step 2, and statistics of the data of various ore-controlling elements of the target layer;
步骤3.1、确定步骤1.2中圈定的重点地区边界,在前人研究成果的基础上利用Mapgis软件修编重点地区地质图,并制作重点地区边界拐点坐标表格;步骤3.2、依据大量钻孔资料,统计步骤2中厘定出的有利成矿目标层位的地层厚度、底板埋深、砂体厚度、砂地比、氧化砂体厚度、还原砂体厚度等控矿要素数据及其钻孔坐标,统计整理为表格形式;Step 3.1, determine the boundary of key areas delineated in step 1.2, use Mapgis software to edit the geological map of key areas on the basis of previous research results, and make a table of coordinates of inflection points of the boundaries of key areas; step 3.2, based on a large number of drilling data, statistics The ore-controlling element data and drilling coordinates of the favorable ore-forming target layers determined in step 2, such as stratum thickness, floor burial depth, sand body thickness, sand-to-ground ratio, oxidized sand body thickness, and reduced sand body thickness, are statistically organized as form form;
步骤3.3、在上述步骤的基础上,将重点地区边界坐标分别与步骤3.2中各控矿要素统计数据合并,并且将重点地区边界坐标赋值为0,按控矿要素分别整理成独立表格备用。Step 3.3. On the basis of the above steps, the boundary coordinates of the key areas are merged with the statistical data of the ore-controlling elements in step 3.2, and the boundary coordinates of the key areas are assigned a value of 0, and the ore-controlling elements are sorted into separate tables for future use.
所述步骤4:利用Surfer软件绘制目标层位各控矿要素图件,筛选各要素最有利成矿区间;Said step 4: using Surfer software to draw maps of each ore-controlling element in the target layer, and screening the most favorable ore-forming interval for each element;
步骤4.1、利用Surfer软件将步骤3.3中的数据导入软件,绘制目标层位各要素等值线图;Step 4.1, utilize Surfer software to import the data in step 3.3 into the software, and draw the contour map of each element of the target layer;
步骤4.2、利用钻孔资料,识别目标层相标志,修编目标层位的沉积相展布图。Step 4.2: Utilize the drilling data to identify the target stratum facies mark, and edit the sedimentary facies distribution map of the target stratum.
步骤4.3、根据前期现有研究资料,总结典型砂岩型铀矿床有利成矿要素区间阀值,划定有利成矿要素最有利成矿区间;Step 4.3. Based on the existing research data in the previous period, summarize the threshold value of the favorable ore-forming elements interval of typical sandstone-type uranium deposits, and delineate the most favorable ore-forming interval of the favorable ore-forming elements;
步骤4.4、根据步骤4.2中的标准,筛选各要素最有利成矿区间,其中,地层厚度>80m,底板埋深<1000m,砂体厚度≥60m,砂地比≥0.5,还原砂体10-50m最佳,其次为50-70m,氧化砂体厚度10-40m。Step 4.4. According to the criteria in step 4.2, screen the most favorable ore-forming intervals for each element, among which, the stratum thickness > 80m, the floor depth < 1000m, the sand body thickness ≥ 60m, the sand-to-ground ratio ≥ 0.5, and the reduced sand body 10-50m most Good, followed by 50-70m, and the thickness of oxidized sand body is 10-40m.
步骤5:对各类图件套合叠置,精确定位有利铀成矿砂体;Step 5: Overlap all kinds of maps and accurately locate favorable uranium ore-forming sand bodies;
步骤5.1、利用Mapgis或CorelDRAW软件对步骤4.3中的筛选出的最有利成矿区间的各要素图件在沉积相底图中进行套合叠置;Step 5.1, use Mapgis or CorelDRAW software to nest and superimpose each element map of the most favorable metallogenic interval screened out in step 4.3 in the sedimentary facies base map;
步骤5.2、在步骤5.1的基础上,依据各有利要素重合的概率,划定重合80%以上的区域为最有利成矿砂体,重合65-80%的区域次之。Step 5.2: On the basis of step 5.1, according to the probability of the coincidence of each favorable element, delineate the area with an overlap of more than 80% as the most favorable ore-forming sand body, followed by the area with an overlap of 65-80%.
本发明的有益效果:Beneficial effects of the present invention:
本发明方法在对重点盆段(地区)深度分析的基础上整合、统计大量钻孔数据编制有利成矿要素系列图件,提取各有利成矿要素最有利成矿区间进行套合叠置,从而精确定位覆盖区下有利铀成矿砂体分布特征,为后续找矿工作提供有利支撑。The method of the present invention integrates and counts a large amount of drilling data on the basis of depth analysis of key basin segments (regions) to compile a series of maps of favorable metallogenic elements, extracts the most favorable metallogenic intervals of each favorable metallogenic elements, and nests and superimposes them, thereby Precisely locating the distribution characteristics of favorable uranium ore-forming sand bodies under the coverage area provides favorable support for subsequent ore prospecting work.
本发明在层序地层学、沉积岩石学、铀矿地质、岩性地球化学特征等理论指导下,利用大量钻孔数据编制系列有利成矿要素图,数据来源真实可靠,图件具有较高的准确度。此外,根据现有技术资料划分的最有利成矿要素区间,对编制的图件进行筛选叠合,从而厘定出有利成矿砂体的分布情况。本发明方法对有利成矿砂体的圈定具有实际指导意义,准确性较高,能够直接指导实际找矿工作,解决有利成矿砂体定位预测关键技术;此外,也可用于评价某一地区的铀矿潜力、预测资源量。Under the guidance of theories of sequence stratigraphy, sedimentary petrology, uranium geology, and lithologic geochemical characteristics, the present invention uses a large number of drilling data to compile a series of maps of favorable ore-forming elements. The data sources are true and reliable, and the maps have high Accuracy. In addition, according to the most favorable ore-forming element intervals divided by the existing technical data, the compiled maps were screened and superimposed to determine the distribution of favorable ore-forming sand bodies. The method of the invention has practical guiding significance for the delineation of favorable ore-forming sand bodies, has high accuracy, can directly guide the actual ore prospecting work, and solves the key technology of favorable ore-forming sand body location prediction; in addition, it can also be used to evaluate uranium deposits in a certain area Potential and estimated resource volume.
附图说明Description of drawings
图1为本发明设计的覆盖区有利铀成矿砂体的精确定位方法流程框图;Fig. 1 is a block diagram of the accurate positioning method for favorable uranium ore-forming sand bodies in the coverage area designed by the present invention;
图2为本发明所述实施例中有利成矿砂体定位图。Fig. 2 is a location map of favorable ore-forming sand bodies in the embodiment of the present invention.
具体实施方式Detailed ways
下面结合附图和实施例对本发明的一种覆盖区有利铀成矿砂体的精确定位方法进行详细说明。A method for accurately positioning favorable uranium ore-forming sand bodies in the coverage area of the present invention will be described in detail below in conjunction with the accompanying drawings and embodiments.
一种覆盖区有利铀成矿砂体的精确定位方法,包括如下步骤:A method for precisely locating favorable uranium ore-forming sand bodies in an overlay area, comprising the following steps:
步骤1、收集、分析资料,圈定具有较大潜力重点找矿盆段、地区;Step 1. Collect and analyze data, delineate key prospecting basins and areas with great potential;
步骤1.1、初步圈定重点盆段;Step 1.1. Preliminary delineation of key basin segments;
步骤1.2、在步骤1.1圈定的重点找矿盆段基础上,圈定重点地区;Step 1.2, on the basis of the key prospecting basin sections delineated in step 1.1, delineate key areas;
步骤2、厘定有利找矿目标层位;Step 2. Determine the favorable prospecting target layer;
步骤3、补充收集钻穿步骤2中厘定的有利找矿目标层位的钻孔资料,统计目标层位各类控矿要素的数据;Step 3. Supplementary collection of drilling data for drilling through the favorable ore prospecting target layer determined in step 2, and statistics of data on various ore-controlling elements of the target layer;
步骤4、利用Surfer软件绘制目标层位各控矿要素图件,筛选各要素最有利成矿区间;Step 4, use Surfer software to draw the map of each ore-controlling element in the target layer, and screen the most favorable mineralization interval of each element;
步骤5、对各类图件套合叠置,精确定位有利铀成矿砂体。Step 5. Overlap and overlay all kinds of maps to accurately locate favorable uranium ore-forming sand bodies.
所述步骤1.1、初步圈定重点盆段,包括:收集研究盆地的区域地质、大地构造演化等图文资料,明确盆地类型、沉积盖层、基底岩性、蚀源区条件等要素,按照一级构造单元圈定具有较大潜力重点找矿盆段:The step 1.1, preliminary delineation of key basin sections, includes: collecting graphic data such as regional geology and tectonic evolution of the research basin, clarifying elements such as basin type, sedimentary cover, basement lithology, erosion source area conditions, etc., according to the first-level Structural units delineate key prospecting basins with great potential:
所述挤压盆地类型一级构造单元以山前斜坡带、裂陷盆地类型一级构造单元以隆起区为首选;The first-order structural unit of the extrusion basin type is the piedmont slope belt, and the first-order structural unit of the rift basin type is the uplift area;
所述沉积盖层以发育层间氧化带且厚度<1000m为有利;It is favorable for the sedimentary cover layer to develop an interlayer oxidation zone with a thickness <1000m;
所述蚀源区岩性花岗岩为首选,火山碎屑岩、酸性火山岩次之,铀含量≥5ppm。Lithological granite in the erosion source area is the first choice, followed by pyroclastic rock and acidic volcanic rock, with uranium content ≥ 5ppm.
所述步骤1.2在步骤1.1圈定的重点找矿盆段基础上,圈定重点地区,包括:着重收集整理该盆段地质、构造、地震数据,研究分析该盆段沉积体系、古气候演化、物源—铀源供给条件等要素,划分二级构造单元并据此进一步圈定有利成矿重点地区:依据步骤1.1中有利沉积盖层厚度在垂向上界定有利成矿地质年代范围;整合前期现有研究资料、分析该盆段古气候、沉积演化特征,确定垂向上以半干旱—半潮湿气候条件、沉积体系以河流—三角洲体系为有利;综合上述有利要素,以二级构造单元为单位,横向上保证物源—铀源供给充足,以靠近物源区、蚀源区或构造剥蚀区为有利,进而综合研判圈定有利成矿重点地区。The step 1.2 delineates the key areas on the basis of the key prospecting basins delineated in step 1.1, including: focusing on collecting and sorting out the geological, structural, and seismic data of the basins, and researching and analyzing the sedimentary system, paleoclimate evolution, and provenance of the basins — Uranium source supply conditions and other factors, divide the secondary structural units and further delineate the key areas of favorable mineralization: according to the thickness of the favorable sedimentary cap rock in step 1.1, define the range of favorable mineralization geological age vertically; integrate the existing research data in the previous period 1. Analyze the paleoclimate and sedimentary evolution characteristics of this basin section, and determine that the semi-arid-semi-humid climate conditions in the vertical direction and the river-delta system in the sedimentary system are favorable; Provenance—uranium source is sufficient, and it is advantageous to be close to the provenance area, erosion source area or structural denudation area, and then comprehensively study and judge to delineate the key areas of favorable mineralization.
步骤2、厘定有利找矿目标层位包括:Step 2. Determining favorable prospecting target layers includes:
步骤2.1、在步骤1圈定的重点地区范围内,收集钻孔资料,所述收集钻孔资料覆盖全区的地震剖面等资料;Step 2.1, within the key areas delineated in step 1, collect borehole data, and the collected borehole data cover the seismic profiles and other data in the whole area;
步骤2.2、垂向上,利用钻孔数据资料建立多个典型单井柱状图,结合区域上的地震剖面等资料明确地层厚度,建立该重点地区综合柱状图;在此基础上对各地层间、层组内的岩性结构进行分析,结合前期现有研究成果优选垂向上有利岩性组合以发育稳定的泥-砂-泥结构为主的地层;Step 2.2, vertically, use the drilling data to establish multiple typical single-well histograms, combine the regional seismic profile and other data to clarify the stratum thickness, and establish a comprehensive histogram for this key area; Based on the analysis of the lithological structure within the formation, combined with the previous research results, the vertically favorable lithological combination is selected to develop a stable mud-sand-mud structure;
步骤2.3、横向上,绘制连井剖面,以层组为单位进一步划分沉积相带、砂体发育、层间氧化带等要素、确定以辫状河流相、曲流河河道亚相、辫状河三角洲相平原亚相;发育多层砂体且单层砂体厚度在5-15m,连续性较好;层间氧化带发育规模大的层位为有利目标层位。Step 2.3. Horizontally, draw the well-connected section, further divide the sedimentary facies belt, sand body development, interlayer oxidation zone and other elements in units of formations, and determine the braided fluvial facies, meandering river channel subfacies, and braided fluvial facies. Delta facies plain subfacies; multi-layer sand bodies are developed and the thickness of a single layer of sand bodies is 5-15m, with good continuity; the layers with large-scale development of interlayer oxidation zones are favorable target layers.
所述步骤3、补充收集钻穿步骤2中厘定的有利找矿目标层位的钻孔资料,统计目标层位各类控矿要素的数据;The step 3, supplementary collection of drilling data for drilling through the favorable ore prospecting target layer determined in step 2, and statistics of the data of various ore-controlling elements of the target layer;
步骤3.1、确定步骤1.2中圈定的重点地区边界,在前人研究成果的基础上利用Mapgis软件修编重点地区地质图,并制作重点地区边界拐点坐标表格;步骤3.2、依据大量钻孔资料,统计步骤2中厘定出的有利成矿目标层位的地层厚度、底板埋深、砂体厚度、砂地比、氧化砂体厚度、还原砂体厚度等控矿要素数据及其钻孔坐标,统计整理为表格形式;Step 3.1, determine the boundary of key areas delineated in step 1.2, use Mapgis software to edit the geological map of key areas on the basis of previous research results, and make a table of coordinates of inflection points of the boundaries of key areas; step 3.2, based on a large number of drilling data, statistics The ore-controlling element data and drilling coordinates of the favorable ore-forming target layers determined in step 2, such as stratum thickness, floor burial depth, sand body thickness, sand-to-ground ratio, oxidized sand body thickness, and reduced sand body thickness, are statistically organized as form form;
步骤3.3、在上述步骤的基础上,将重点地区边界坐标分别与步骤3.2中各控矿要素统计数据合并,并且将重点地区边界坐标赋值为0,按控矿要素分别整理成独立表格备用。Step 3.3. On the basis of the above steps, the boundary coordinates of the key areas are merged with the statistical data of the ore-controlling elements in step 3.2, and the boundary coordinates of the key areas are assigned a value of 0, and the ore-controlling elements are sorted into separate tables for future use.
所述步骤4:利用Surfer软件绘制目标层位各控矿要素图件,筛选各要素最有利成矿区间;Said step 4: using Surfer software to draw maps of each ore-controlling element in the target layer, and screening the most favorable ore-forming interval for each element;
步骤4.1、利用Surfer软件将步骤3.3中的数据导入软件,绘制目标层位各要素等值线图;Step 4.1, utilize Surfer software to import the data in step 3.3 into the software, and draw the contour map of each element of the target layer;
步骤4.2、利用钻孔资料,识别目标层相标志,修编目标层位的沉积相展布图。Step 4.2: Utilize the drilling data to identify the target stratum facies mark, and edit the sedimentary facies distribution map of the target stratum.
步骤4.3、根据前期现有研究资料,总结典型砂岩型铀矿床有利成矿要素区间阀值,划定有利成矿要素最有利成矿区间;Step 4.3. Based on the existing research data in the previous period, summarize the threshold value of the favorable ore-forming elements interval of typical sandstone-type uranium deposits, and delineate the most favorable ore-forming interval of the favorable ore-forming elements;
步骤4.4、根据步骤4.2中的标准,筛选各要素最有利成矿区间,其中,地层厚度>80m,底板埋深<1000m,砂体厚度≥60m,砂地比≥0.5,还原砂体10-50m最佳,其次为50-70m,氧化砂体厚度10-40m。Step 4.4. According to the criteria in step 4.2, screen the most favorable ore-forming intervals for each element, among which, the stratum thickness > 80m, the floor depth < 1000m, the sand body thickness ≥ 60m, the sand-to-ground ratio ≥ 0.5, and the reduced sand body 10-50m most Good, followed by 50-70m, and the thickness of oxidized sand body is 10-40m.
步骤5:对各类图件套合叠置,精确定位有利铀成矿砂体;Step 5: Overlap all kinds of maps and accurately locate favorable uranium ore-forming sand bodies;
步骤5.1、利用Mapgis或CorelDRAW软件对步骤4.3中的筛选出的最有利成矿区间的各要素图件在沉积相底图中进行套合叠置;Step 5.1, use Mapgis or CorelDRAW software to nest and superimpose each element map of the most favorable metallogenic interval screened out in step 4.3 in the sedimentary facies base map;
步骤5.2、在步骤5.1的基础上,依据各有利要素重合的概率,划定重合80%以上的区域为最有利成矿砂体,重合65-80%的区域次之。Step 5.2: On the basis of step 5.1, according to the probability of the coincidence of each favorable element, delineate the area with an overlap of more than 80% as the most favorable ore-forming sand body, followed by the area with an overlap of 65-80%.
上面对本发明的实施例作了详细说明,本发明并不限于上述实例,在本领域普通技术人员所具备的知识范围内,还可以在不脱离本发明宗旨的前提下做出各种变化。The embodiments of the present invention have been described in detail above, and the present invention is not limited to the above examples, and various changes can be made within the knowledge of those skilled in the art without departing from the gist of the present invention.
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