科皮特科夫斯基磷矿数字构造岩性模型及地质成因特征

D. Khrushchov, O. Remezova, S. Vasylenko, O. Shevchuk, O. Yaremenko
{"title":"科皮特科夫斯基磷矿数字构造岩性模型及地质成因特征","authors":"D. Khrushchov, O. Remezova, S. Vasylenko, O. Shevchuk, O. Yaremenko","doi":"10.26565/2410-7360-2022-56-06","DOIUrl":null,"url":null,"abstract":"Introduction. The relevance of this publication is associated with the problem of foundation and developing a raw material base of phosphate raw material in accordance with the demand of the national agro-industrial complex.\n\nThe purpose of the publication is to develop a preliminary digital structural-lithological model (DSLM) of the Kopytkivsky deposit, as a tool for information support of its development, as well as geological and genetic characteristics of the object as a basis for specifying the criteria for predicting deposits of this type.\n\nThis goal covers the following tasks: - presentation of methodology and research methods; - presentation of the database; - demonstration of derivatives of the created digital structural-lithological model (DSLM) and their interpretation;- representation of functional and cognitive characteristics of the object (Kopytkivsky phosphorite deposit).\n\nMaterials and Metodology. The studies are based on two methodological principles: traditional lithological, paleofacial, paleogeographic studies and the author's development - digital structural and lithological modeling, dialectically combined in the form of a single predictive-paleoreconstructive retrospective-static model.\n\nMain Results. Kopytkivsky deposit belongs to the Zdolbunovskiy district of the Zdolbunovskiy-Ternopil zone of the Volyn-Podolsk Cretaceous basin of the phosphorite-bearing province of the East European platform. The indicated zone refers to the Volyno-Podilllya plate, i.e the western slope of the Ukrainian shield. In the area of the Kopytkivsky deposit, layers of inoceramic limestones represent the lower stratigraphic subdivision of the Cretaceous system, lying directly on the pre-Mesozoic basement. The DSLM of the Kopytkivsky field has been developed, intended for information support for further work on its development (detailed exploration and operation). The DSLM database is represented by a description of 567 geological exploration wells.\n\nConclusions. Based on the constructed DSLM, a number of derivatives (including visualizations) were obtained that reflect the structural and material - industrial characteristics of the field - a number of maps, profiles, as well as a block diagram of the central part of the field. The description of the most informative visualizations are given: Map of the hypsometry of the bottom of the \"productive horizon\", Map of the hypsometry of the roof of the \"productive horizon\", Map of specific reserves and others. The model derivatives reflect the spatial (areal and hypsometric) configuration of phosphorites ore bodies and the distribution of specific reserves of P2O5. Based on the methodological principles of formation analysis and the methodological approaches adopted by us for predictive-paleoreconstructive retrospective-static modeling of the object, a geological and genetic characteristic of the stage of formation of layers of inoceramic limestones has been obtained. The mechanism of phosphorite formation is considered. The presented DSLM is intended for information support of detailed and operational exploration, with the prospect of the current development of the model (as a permanent one) with the addition of new data during exploration and operational work.","PeriodicalId":52802,"journal":{"name":"Visnik Kharkivs''kogo natsional''nogouniversitetu imeni VN Karazina Seriia Radiofizika ta elektronika","volume":"197 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Digital structural-lithological model and geological-genetic characteristics of Kopytkovsky phosphorite deposit\",\"authors\":\"D. Khrushchov, O. Remezova, S. Vasylenko, O. Shevchuk, O. Yaremenko\",\"doi\":\"10.26565/2410-7360-2022-56-06\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Introduction. The relevance of this publication is associated with the problem of foundation and developing a raw material base of phosphate raw material in accordance with the demand of the national agro-industrial complex.\\n\\nThe purpose of the publication is to develop a preliminary digital structural-lithological model (DSLM) of the Kopytkivsky deposit, as a tool for information support of its development, as well as geological and genetic characteristics of the object as a basis for specifying the criteria for predicting deposits of this type.\\n\\nThis goal covers the following tasks: - presentation of methodology and research methods; - presentation of the database; - demonstration of derivatives of the created digital structural-lithological model (DSLM) and their interpretation;- representation of functional and cognitive characteristics of the object (Kopytkivsky phosphorite deposit).\\n\\nMaterials and Metodology. The studies are based on two methodological principles: traditional lithological, paleofacial, paleogeographic studies and the author's development - digital structural and lithological modeling, dialectically combined in the form of a single predictive-paleoreconstructive retrospective-static model.\\n\\nMain Results. Kopytkivsky deposit belongs to the Zdolbunovskiy district of the Zdolbunovskiy-Ternopil zone of the Volyn-Podolsk Cretaceous basin of the phosphorite-bearing province of the East European platform. The indicated zone refers to the Volyno-Podilllya plate, i.e the western slope of the Ukrainian shield. In the area of the Kopytkivsky deposit, layers of inoceramic limestones represent the lower stratigraphic subdivision of the Cretaceous system, lying directly on the pre-Mesozoic basement. The DSLM of the Kopytkivsky field has been developed, intended for information support for further work on its development (detailed exploration and operation). The DSLM database is represented by a description of 567 geological exploration wells.\\n\\nConclusions. Based on the constructed DSLM, a number of derivatives (including visualizations) were obtained that reflect the structural and material - industrial characteristics of the field - a number of maps, profiles, as well as a block diagram of the central part of the field. The description of the most informative visualizations are given: Map of the hypsometry of the bottom of the \\\"productive horizon\\\", Map of the hypsometry of the roof of the \\\"productive horizon\\\", Map of specific reserves and others. The model derivatives reflect the spatial (areal and hypsometric) configuration of phosphorites ore bodies and the distribution of specific reserves of P2O5. Based on the methodological principles of formation analysis and the methodological approaches adopted by us for predictive-paleoreconstructive retrospective-static modeling of the object, a geological and genetic characteristic of the stage of formation of layers of inoceramic limestones has been obtained. The mechanism of phosphorite formation is considered. The presented DSLM is intended for information support of detailed and operational exploration, with the prospect of the current development of the model (as a permanent one) with the addition of new data during exploration and operational work.\",\"PeriodicalId\":52802,\"journal\":{\"name\":\"Visnik Kharkivs''kogo natsional''nogouniversitetu imeni VN Karazina Seriia Radiofizika ta elektronika\",\"volume\":\"197 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-06-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Visnik Kharkivs''kogo natsional''nogouniversitetu imeni VN Karazina Seriia Radiofizika ta elektronika\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.26565/2410-7360-2022-56-06\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Visnik Kharkivs''kogo natsional''nogouniversitetu imeni VN Karazina Seriia Radiofizika ta elektronika","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26565/2410-7360-2022-56-06","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

介绍。本出版物的相关性与根据国家农工综合体的需求建立和发展磷酸盐原料原料基地的问题有关。该出版物的目的是开发Kopytkivsky矿床的初步数字构造-岩性模型(DSLM),作为其开发的信息支持工具,以及该对象的地质和遗传特征,作为指定预测此类矿床的标准的基础。这一目标包括以下任务:-介绍方法和研究方法;-数据库的介绍;-演示创建的数字结构-岩性模型(DSLM)的衍生品及其解释;-表示对象(Kopytkivsky磷矿床)的功能和认知特征。材料和方法。研究基于两种方法论原则:传统的岩性、古面相、古地理研究和作者开发的数字构造和岩性模拟,以单一的预测-古构造-回溯-静态模式辩证地结合起来。主要的结果。Kopytkivsky矿床属于东欧地台含磷省Volyn-Podolsk白垩纪盆地Zdolbunovskiy- ternopil带的Zdolbunovskiy区。所示区域指的是Volyno-Podilllya板块,即乌克兰地盾的西坡。在Kopytkivsky矿床地区,陶粒灰岩层代表了白垩纪体系的下地层细分,直接位于前中生代基底上。Kopytkivsky油田的DSLM已经开发,目的是为进一步的开发工作(详细勘探和操作)提供信息支持。DSLM数据库由567口地质勘探井的描述来表示。基于构建的DSLM,获得了反映该领域结构和材料-工业特征的许多衍生物(包括可视化)-许多地图,剖面图以及该领域中心部分的方框图。给出了最具信息量的可视化描述:“生产水平”底部的低斜视图,“生产水平”顶部的低斜视图,特定储量图等。模型导数反映了磷矿矿体的空间(面)构型和P2O5比储量的分布。根据地层分析的方法学原理和我们采用的预测-古重建-回溯-静态建模方法,获得了陶粒灰岩层形成阶段的地质和成因特征。探讨了磷矿的形成机理。所提出的DSLM旨在为详细的和可操作的勘探提供信息支持,并展望该模型的当前发展(作为永久模型),在勘探和操作工作期间增加新的数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Digital structural-lithological model and geological-genetic characteristics of Kopytkovsky phosphorite deposit
Introduction. The relevance of this publication is associated with the problem of foundation and developing a raw material base of phosphate raw material in accordance with the demand of the national agro-industrial complex. The purpose of the publication is to develop a preliminary digital structural-lithological model (DSLM) of the Kopytkivsky deposit, as a tool for information support of its development, as well as geological and genetic characteristics of the object as a basis for specifying the criteria for predicting deposits of this type. This goal covers the following tasks: - presentation of methodology and research methods; - presentation of the database; - demonstration of derivatives of the created digital structural-lithological model (DSLM) and their interpretation;- representation of functional and cognitive characteristics of the object (Kopytkivsky phosphorite deposit). Materials and Metodology. The studies are based on two methodological principles: traditional lithological, paleofacial, paleogeographic studies and the author's development - digital structural and lithological modeling, dialectically combined in the form of a single predictive-paleoreconstructive retrospective-static model. Main Results. Kopytkivsky deposit belongs to the Zdolbunovskiy district of the Zdolbunovskiy-Ternopil zone of the Volyn-Podolsk Cretaceous basin of the phosphorite-bearing province of the East European platform. The indicated zone refers to the Volyno-Podilllya plate, i.e the western slope of the Ukrainian shield. In the area of the Kopytkivsky deposit, layers of inoceramic limestones represent the lower stratigraphic subdivision of the Cretaceous system, lying directly on the pre-Mesozoic basement. The DSLM of the Kopytkivsky field has been developed, intended for information support for further work on its development (detailed exploration and operation). The DSLM database is represented by a description of 567 geological exploration wells. Conclusions. Based on the constructed DSLM, a number of derivatives (including visualizations) were obtained that reflect the structural and material - industrial characteristics of the field - a number of maps, profiles, as well as a block diagram of the central part of the field. The description of the most informative visualizations are given: Map of the hypsometry of the bottom of the "productive horizon", Map of the hypsometry of the roof of the "productive horizon", Map of specific reserves and others. The model derivatives reflect the spatial (areal and hypsometric) configuration of phosphorites ore bodies and the distribution of specific reserves of P2O5. Based on the methodological principles of formation analysis and the methodological approaches adopted by us for predictive-paleoreconstructive retrospective-static modeling of the object, a geological and genetic characteristic of the stage of formation of layers of inoceramic limestones has been obtained. The mechanism of phosphorite formation is considered. The presented DSLM is intended for information support of detailed and operational exploration, with the prospect of the current development of the model (as a permanent one) with the addition of new data during exploration and operational work.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
审稿时长
8 weeks
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信