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Journal articles on the topic 'Geochemical background'

Author: Grafiati

Published: 8 June 2024

Last updated: 31 July 2025

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1

Gałuszka, Agnieszka, and Zdzisław Migaszewski. "Geochemical background - an environmental perspective." Mineralogia 42, no. 1 (2011): 7–17. http://dx.doi.org/10.2478/v10002-011-0002-y.

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Geochemical background - an environmental perspectiveThis article presents the concept of geochemical background from an environmental perspective. The idea of establishing the typical concentrations of elements in various environmental compartments, proposed by exploratory geochemists almost 50 years ago was important for the detection of anomalous element concentrations, thus providing a basic tool in the search for new mineral deposits. At present, the knowledge of the geochemical background of hazardous elements is essential for: defining pollution, identifying the source of contamination,

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Cembranel, Adir S., Silvio C. Sampaio, Marcelo B. Remor, Jackeline T. Gotardo, and Pábolla M. Dalla Rosa. "GEOCHEMICAL BACKGROUND IN AN OXISOL." Engenharia Agrícola 37, no. 3 (2017): 565–73. http://dx.doi.org/10.1590/1809-4430-eng.agric.v37n3p565-573/2017.

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Reimann, Clemens, and Robert G. Garrett. "Geochemical background—concept and reality." Science of The Total Environment 350, no. 1-3 (2005): 12–27. http://dx.doi.org/10.1016/j.scitotenv.2005.01.047.

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Matschullat, J., R. Ottenstein, and C. Reimann. "Geochemical background - can we calculate it?" Environmental Geology 39, no. 9 (2000): 990–1000. http://dx.doi.org/10.1007/s002549900084.

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Wen, Weiji, Fan Yang, Shuyun Xie, et al. "Determination of Geochemical Background and Baseline and Research on Geochemical Zoning in the Desert and Sandy Areas of China." Applied Sciences 14, no. 22 (2024): 10612. http://dx.doi.org/10.3390/app142210612.

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Resources in deserts and sandy landscapes have potential for development, but existing surveys and sampling have not collected desert soil samples. As such, the geochemical background of these spaces remains unexplored due to the vastness and desolation of deserts. Therefore, researching the geochemical background values and geochemical baseline values of deserts is of long-term significance. Our research indicates that in addition to macrostructural environmental divisions, microelement geochemistry can also be used for geological unit zoning. In this paper, geochemical background and geochem

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Matschullat, Jörg, Silke Höfle, Juscimar da Silva, et al. "A soil geochemical background for northeastern Brazil." Geochemistry: Exploration, Environment, Analysis 12, no. 3 (2012): 197–209. http://dx.doi.org/10.1144/1467-7873/10-ra-046.

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Vodianitsky, Yu, N. Kosareva, and A. Savichev. "LANTANIDES (Y, La, Ce, Pr, Nd, Sm) AND ACTINIDS (Th, U) IN SOILS OF THE HIBINO-LOVOZERO PROVINCE." Dokuchaev Soil Bulletin, no. 65 (June 30, 2010): 75–86. http://dx.doi.org/10.19047/0136-1694-2010-65-75-86.

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In the Khibinsko-Lovozero district of the Kola Peninsula, the territory is divided into three geochemically different areas. In the background area near Umbozero, both mineral and peated samples contain all rare metals below clark: lanthanides and actinides are leaching heavily from acidic podzolic soils. В in the area of weak geochemical anomaly (near Lovozero), all lanthanides are inherited from the loparite-containing rock, and all actinides - Th: their content is 1.3-5.4 times higher than the clark value. In the zone of a strong geochemical anomaly (on the northern shore of Seidozero and o

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Garrett, Robert G., Gerald C. Lalor, John Preston, and M. K. Vutchkov. "Variation in geochemical background levels for Jamaican soils." Geochemistry: Exploration, Environment, Analysis 8, no. 2 (2008): 149–56. http://dx.doi.org/10.1144/1467-7873/07-158.

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Zhou, Di. "Adjustment of geochemical background by robust multivariate statistics." Journal of Geochemical Exploration 24, no. 2 (1985): 207–22. http://dx.doi.org/10.1016/0375-6742(85)90046-9.

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Liu, Rui Ping, You Ning Xu, Fang He, et al. "Environmental Impact by Heavy-Metal Dispersion from the Fine Sediments of the Shuangqiao River, Xiaoqinling Gold Area, China." Advanced Materials Research 518-523 (May 2012): 1929–35. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.1929.

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Abstract. the sediments is the second pollution source to the water quality of river in mining area, in order to assess the pollution extent of the Shuangqiao River by anthropogenic activity, and establish the geochemical background values and the possible geochemical anomaly range, The authors use Lognormal distribution plots to study the Mercury, Chromium, Cadmium, Lead, Copper, Arsenic, Zinc and Iron dispersion in the fine sediments of the Shuangqiao River. The Lognormal distribution plots are applied to discriminate the geochemical background levels of eight heavy metals from the geochemic

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Chen, Lirong, Qingfeng Guan, Bin Feng, Hanqiu Yue, Junyi Wang, and Fan Zhang. "A Multi-Convolutional Autoencoder Approach to Multivariate Geochemical Anomaly Recognition." Minerals 9, no. 5 (2019): 270. http://dx.doi.org/10.3390/min9050270.

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The spatial structural patterns of geochemical backgrounds are often ignored in geochemical anomaly recognition, leading to the ineffective recognition of valuable anomalies in geochemical prospecting. In this contribution, a multi-convolutional autoencoder (MCAE) approach is proposed to deal with this issue, which includes three unique steps: (1) a whitening process is used to minimize the correlations among geochemical elements, avoiding the diluting of effective background information embedded in redundant data; (2) the Global Moran’s I index is used to determine the recognition domain of t

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Zinkutė, Rimantė, Ričardas Taraškevičius, Margarita Jankauskaitė, Vaidotas Kazakauskas, and Žilvinas Stankevičius. "Influence of site-classification approach on geochemical background values." Open Chemistry 18, no. 1 (2020): 1391–411. http://dx.doi.org/10.1515/chem-2020-0177.

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AbstractThis study of peri-urban minerogenic topsoil on glacigenic or post-glacial deposits shows the influence of the site-classification approach on the differentiated median background (DMB) values of major elements and the potentially harmful elements (PHEs) Ba, Cr, Cu, Mn, Ni, Pb and Zn. Composite samples from forests and meadows were taken in 25 sites, each of which had five sub-sites. A fraction of <2 mm was used to determine the organic matter by loss on ignition (LOI), grain size by laser diffraction and the elemental contents by X-ray fluorescence. The following five site-classifi

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Nakić, Zoran, Kristijan Posavec, and Andrea Bačani. "A Visual Basic Spreadsheet Macro for Geochemical Background Analysis." Ground Water 45, no. 5 (2007): 642–47. http://dx.doi.org/10.1111/j.1745-6584.2007.00325.x.

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Li, Peiyu, Qingjie Gong, Shaoyu Chen, et al. "Regional Geochemical Characteristics of Lithium in the Mufushan Area, South China." Applied Sciences 14, no. 5 (2024): 1978. http://dx.doi.org/10.3390/app14051978.

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With the explosive growth in demand for lithium (Li) resources, the Mufushan area has been a hotspot for Li deposit exploration in China in recent years. Geochemical maps and geochemical anomaly maps are basic maps in the geochemical exploration of mineral resources. A fixed-value method to contour a Li geochemical map is presented here, in which Li concentrations are divided into 19 levels on 18 fixed values, ranging from 5 μg/g (corresponding to the detection limit) to 1858 μg/g (corresponding to the cut-off grade of Li deposit in hard-rock type) and illustrated in six color tones correspond

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Xu, Shan, Miao Wang, Chang Chun Liu, and Shou Yi Li. "Evaluation of Gold Geochemical Anomalies in the Liaodong Paleorift." Applied Mechanics and Materials 484-485 (January 2014): 620–27. http://dx.doi.org/10.4028/www.scientific.net/amm.484-485.620.

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89 Au geochemical anomalies are delineated by using 1/200000 regional geochemical exploration data. By researching regional geochemical characteristics and the relationship with the geological background, the author points out that: the main factors causing high background of Au geochemical anomalies are Gaixian and Dashiqiao formation of Liaohe group, intrusions of Mesozoic intermediate-acid intrusive rocks. The elements combination types of typical anomalies are determined by using factorial analysis,cluster analysis and other mathematical methods with the combination of elements association

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Zakharchenko, A. V., O. A. Pasko, A. A. Tigeev, and D. V. Moskovchenko. "On the Background Values of the Geochemical Spectra of Microelements of the Solid Phase of Snow During their Comparative Analysis in the Cities of Tobolsk And Tyumen." Ecology and Industry of Russia 27, no. 4 (2023): 61–65. http://dx.doi.org/10.18412/1816-0395-2023-4-61-65.

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Local features of the geochemical spectra of trace elements in the snow dust of Tobolsk and Tyumen were revealed using a hierarchical cluster analysis of the normalized values of their content. Geochemical spectra of snow sampling points were studied in residential and industrial areas, as well as in significantly remote areas (conditional background). Four clusters were identified in Tobolsk and five in Tyumen, for each of them characteristic geochemical spectra and pollution sources were detected.

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Gregorauskienė, Virgilija. "MAPPING OF GEOCHEMICAL CONTAMINATION IN URBAN AREAS OF LITHUANIA." JOURNAL OF ENVIRONMENTAL ENGINEERING AND LANDSCAPE MANAGEMENT 14, no. 1 (2006): 52–57. http://dx.doi.org/10.3846/16486897.2006.9636879.

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In Lithuania geochemical mapping of urban areas was started in Vilnius city in 1985. Topsoil, stream sediments, snow cover, manufactory dust and other sampling media are used in ecogeochemical investigations. The aim of investigations is to detect sources of pollution, its geochemical properties and spread of its contamination. Furthermore, a sanitary assessment of urban soil is carried out on the basis of available geochemical data and the soil quality standard of Lithuania HN 60:2004. The soil contamination with heavy metals is estimated according to the highest allowable concentrations (HAC

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Salomão, Gabriel Negreiros, Danielle de Lima Farias, Prafulla Kumar Sahoo, Roberto Dall’Agnol, and Dibyendu Sarkar. "Integrated Geochemical Assessment of Soils and Stream Sediments to Evaluate Source-Sink Relationships and Background Variations in the Parauapebas River Basin, Eastern Amazon." Soil Systems 5, no. 1 (2021): 21. http://dx.doi.org/10.3390/soilsystems5010021.

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This study aims to handle an integrated evaluation of soil and stream sediment geochemical data to evaluate source apportionment and to establish geochemical threshold variations for Fe, Al, and 20 selected Potentially Toxic Elements (PTE) in the Parauapebas River Basin (PB), Eastern Amazon. The data set used in this study is from the Itacaiúnas Geochemical Mapping and Background Project (ItacGMBP), which collected 364 surface soil (0–10 cm) samples and 189 stream sediments samples in the entire PB. The <0.177 mm fraction of these samples were analyzed for 51 elements by ICP-MS and ICP-AES,

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Calmus, Thierry, Martín Valencia-Moreno, Rafael Del Río-Salas, Lucas Ochoa-Landín, and Héctor Mendivil-Quijada. "A multi-elemental study to establish the natural background and geochemical anomalies in rocks from the Sonora river upper basin, NW Mexico." Revista Mexicana de Ciencias Geológicas 35, no. 2 (2018): 158–67. http://dx.doi.org/10.22201/cgeo.20072902e.2018.2.605.

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Growing industrialization, including mining activity, dramatically increases environmental pollution. Exploitation of natural resources triggers landscape alteration, inputs of potentially toxic chemical elements to the environment and health diseases. In the case of mining activity, the measure of any associated environmental disturbance requires a geochemical background as a reference frame. Since in Mexico, there is a lack of this type of references in mining districts, the present study took a recent mining spill as an opportunity to establish the geochemical background of the upper Sonora

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Cheng, Qiuming, F. P. Agterberg, and S. B. Ballantyne. "The separation of geochemical anomalies from background by fractal methods." Journal of Geochemical Exploration 51, no. 2 (1994): 109–30. http://dx.doi.org/10.1016/0375-6742(94)90013-2.

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Abdoulatif, ABASS SALEY, MOUNKAILA Mohamed, SALEY Mahamadou, and ELHADJ DAOU Ibrahim. "Pollution Assessment of Heavy Metals As, Cu, Pb and Zn in the Sirba Greenstone Belt Soils (Liptako, Niger)." International Research Journal of Pure and Applied Chemistry 26, no. 1 (2025): 23–37. https://doi.org/10.9734/irjpac/2025/v26i1895.

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The Sirba greenstone belt was Niger's main gold province. Soil geochemical data from the Sirba gold prospecting campaign carried out from 1989 to 1994 by the Japanese International Cooperation, prior to the advent of gold mining in the region were used in this work. The aim of this work was to establish geochemical background and to assess soil pollution for As, Cu, Pb and Zn. Geochemical data from 16,696 soil samples (analyzed by AAS) had been used to define geochemical background. The median method to calculate the threshold value on log-transformed data was used. Geochemical background data

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22

Zhou, Shuya, Qingjie Gong, Zhaochong Zhang, Zhendong Lv, Shaoyu Chen, and Yonglong An. "Innovative Equation for Determining the Geochemical Background Values of Chromium Based on Major Components in Rock–Soil–Sediment Systems." Applied Sciences 15, no. 1 (2024): 182. https://doi.org/10.3390/app15010182.

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The geochemical background value of chromium (Cr) serves as a pivotal factor in environmental assessments and mineral exploration endeavors. Traditionally, geochemical background values have been determined using statistical parameters derived from dataset analysis, though this method may possess inherent limitations. In this study, we introduce a novel equation to calculate the geochemical background value of Cr, based on the premise that major elements can effectively delineate the geochemical background for trace elements. Using a dataset encompassing 791 abundance records from rocks, soils

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Lyuta, N. G. "FEATURES OF HEAVY METALS DISTRIBUTION IN BOTTOM SEDIMENTS OF THE RIVERS OF UKRAINE." Мінеральні ресурси України, no. 1 (March 30, 2018): 28–32. http://dx.doi.org/10.31996/mru.2018.1.28-32.

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The chemical composition of bottom sediments is an important indicator of the ecological state of both water systems and watershed areas, since contaminated bottom sediments are a potential source of secondary pollution of aquatic systems. The analysis of recent publications shows that great attention has been paid to the chemical composition of bottom sediments, however, as a rule, these studies are of a local nature, that is, they cover very small areas. This often raises the issue of criteria for assessing the ecological and geochemical status of bottom sediments, since a small number of sa

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Aksentov, K. I., V. V. Sattarova, A. S. Astakhov, et al. "MERCURY BACKGROUND IN BOTTOM SEDIMENTS OF THE EASTERN ARCTIC." Доклады Российской академии наук. Науки о Земле 511, no. 1 (2023): 93–97. http://dx.doi.org/10.31857/s2686739723600443.

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On the basis of dated bottom sediment cores, layers accumulated in the pre-industrial period were selected. They determine the mercury concentrations, which are the geochemical background for the selected water areas. The variability of mercury concentrations in the sediments of the inner shelf is small (20–30 μg/kg) and can be used as a basis for environmental assessment in the economic development of the Arctic regions.

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Konstantinova, Elizaveta, Tatiana Minkina, Dina Nevidomskaya, et al. "Establishment of regional background for heavy metals in the soils of the Lower Don and the Taganrog Bay coast." E3S Web of Conferences 265 (2021): 03004. http://dx.doi.org/10.1051/e3sconf/202126503004.

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Data on the regional geochemical background and threshold values of heavy metals are required to establish anomalies and assess soil pollution. As a rule, the background values are the average contents of elements in natural undisturbed soils, or the threshold values for the study area, obtained by statistical methods. The aim of the study is to obtain geochemical threshold values of heavy metals in the soils of the Lower Don and the Taganrog Bay coast using different statistical approaches. A total of 86 topsoil samples were collected from the study area. The concentrations of Cr, Mn, Ni, Сu,

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Licht, Otavio. "Geochemical background - what a complex meaning has such a simple expression!" Geochimica Brasiliensis 34, no. 2 (2020): 161–75. http://dx.doi.org/10.21715/gb2358-2812.2020342161.

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The term background was introduced in geochemistry applied to the prospecting of mineral deposits to designate a value, below which the samples would represent normal contents and above which they would be deviations from normality and could represent anomalies related to mineral deposits. In the 1980’s, when the techniques applied in mineral exploration were absorbed by the nascent environmental sciences, the term background was also incorporated with a very similar meaning. However, since its first application, this term has been adopted arbitrarily, without considering the enormous diversit

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Nawrot, Nicole, Ewa Wojciechowska, Muhammad Mohsin, Suvi Kuittinen, Ari Pappinen, and Shahabaldin Rezania. "Trace Metal Contamination of Bottom Sediments: A Review of Assessment Measures and Geochemical Background Determination Methods." Minerals 11, no. 8 (2021): 872. http://dx.doi.org/10.3390/min11080872.

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This paper provides an overview of different methods of assessing the trace metal (TM) contamination status of sediments affected by anthropogenic interference. The geochemical background determination methods are also described. A total of 25 papers covering rivers, lakes, and retention tanks sediments in areas subjected to anthropogenic pressure from the last three years (2019, 2020, and 2021) were analysed to support our examination of the assessment measures. Geochemical and ecotoxicological classifications are presented that may prove useful for sediment evaluation. Among the geochemical

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Santos, Patrícia, Jorge Espinha Marques, Joana Ribeiro, et al. "Geochemistry of Soils from the Surrounding Area of a Coal Mine Waste Pile Affected by Self-Burning (Northern Portugal)." Minerals 13, no. 1 (2022): 28. http://dx.doi.org/10.3390/min13010028.

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Coal mining can generate organic and inorganic contaminants that can be disseminated in the surrounding soils by leaching and/or aerial deposition. This study aims to identify and characterize the physicochemical and geochemical changes promoted in soils from the surrounding area of a self-burning waste pile in an abandoned coal mine. A soil sampling campaign was conducted bordering the waste pile, comprising the main drainage areas as well as the areas uphill. The soils were characterized geochemically for major and trace elements and multivariate statistics was used in combination with geost

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Juchen, Carlos Roberto, Márcio Antônio Vilas Boas, Cristiano Poleto, and Maurício Macedo. "Use of legal reserve areas as geochemical background in hydrosedimentology studies¹." Revista Brasileira de Ciência do Solo 38, no. 6 (2014): 1950–59. http://dx.doi.org/10.1590/s0100-06832014000600029.

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In hydrosedimentology studies the determination of the trace element concentrations at the study site is imperative, since this background can be used to assess the enrichment of sediments with these elements. This enrichment can be the result of the natural process of geological formation or of anthropogenic activities. In the latter case, guidelines are used to indicate the concentrations at which trace elements cause ecotoxicity effects on the environment. Thus, this study used legal reserve areas in the municipality of Toledo, PR, where natural forests are maintained, with no or minimal hu

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Mateja, Gosar, Šajn Robert, Bavec Špela, Gaberšek Martin, Pezdir Valentina, and Miler Miloš. "Geochemical background and threshold for 47 chemical elements in Slovenian topsoil." Geologija 62, no. 1 (2019): 5–57. http://dx.doi.org/10.5474/geologija.2019.001.

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Ding, Song, Dong-Xing Guan, Zhi-Hua Dai, et al. "Nickel bioaccessibility in soils with high geochemical background and anthropogenic contamination." Environmental Pollution 310 (October 2022): 119914. http://dx.doi.org/10.1016/j.envpol.2022.119914.

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Kot, Fyodor S. "The Effect of Natural Geochemical Background on Neurological and Mental Health." Exposure and Health 12, no. 4 (2019): 569–91. http://dx.doi.org/10.1007/s12403-019-00322-y.

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Azri, Chafai, Habib Abida, and Khaled Medhioub. "Geochemical behaviour of the Tunisian background aerosols in Sirocco wind circulations." Advances in Atmospheric Sciences 26, no. 3 (2009): 390–402. http://dx.doi.org/10.1007/s00376-009-0390-8.

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Hamon, R. E., M. J. McLaughlin, R. J. Gilkes, et al. "Geochemical indices allow estimation of heavy metal background concentrations in soils." Global Biogeochemical Cycles 18, no. 1 (2004): n/a. http://dx.doi.org/10.1029/2003gb002063.

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Stanley, Clifford R., and Alastair J. Sinclair. "Anomaly recognition for multi-element geochemical data — A background characterization approach." Journal of Geochemical Exploration 29, no. 1-3 (1987): 333–53. http://dx.doi.org/10.1016/0375-6742(87)90085-9.

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van den Oever, F. "Aruba - a geochemical baseline study." Netherlands Journal of Geosciences - Geologie en Mijnbouw 79, no. 4 (2000): 467–77. http://dx.doi.org/10.1017/s001677460002196x.

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AbstractA stream-sediment survey was carried out for the island of Aruba. Concentrations in stream sediments represent the abundance of chemical elements in the drainage basins. A geochemical atlas was created from the collected data and natural background values were established. Cluster analysis and pattern recognition techniques were used to gain a better understanding of the data set.Two cluster models were selected to study the various geochemical controls on the sediments and to establish a spatial basis of environmental-quality settings for the development of future environmental polici

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Dziuba, Ekaterina A. "DETERMINATION OF LOCAL BACKGROUND CONTENT OF SOME MACRO- AND MICROELEMENTS IN THE SOILS OF THE PERM REGION." Географический вестник = Geographical bulletin, no. 1 (56) (2021): 95–108. http://dx.doi.org/10.17072/2079-7877-2021-1-95-108.

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According to the V.I. Vernadsky law, chemical elements are distributed unevenly in natural objects. Knowledge of the content of chemical elements in a particular area helps in solving various environmental problems. As a result of economic activity, there occurs anthropogenic transformation of the natural environment, including changes in the geochemical properties of landscapes. For an objective assessment of the anthropogenic impact when studying various territories, it is necessary to take into account the background content of macro- and microelements. Since there is a constant anthropogen

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Tao, Zhongping, Bingli Liu, Ke Guo, et al. "3D Primary Geochemical Halo Modeling and Its Application to the Ore Prediction of the Jiama Polymetallic Deposit, Tibet, China." Geofluids 2021 (August 19, 2021): 1–13. http://dx.doi.org/10.1155/2021/6629187.

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The identification of primary geochemical haloes can be used to predict mineral resources in deep-seated orebodies through the delineation of element distributions. The Jiama deposits a typical skarn–porphyry Cu–polymetallic deposit in the Gangdese metallogenic belt of Tibet. The Cu–polymetallic skarn, Cu–Mo hornfels, and Mo ± Cu porphyry mineralization there exhibit superimposed geochemical haloes at depth. Three-dimensional (3D) primary geochemical halo modeling was undertaken for the deposit with the aim of providing geochemical data to describe element distributions in 3D space. An overall

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Oreshkin, Valentin, and Vladislav Khrisanov. "ON THE PREVALENCE OF BACKGROUND AND TECHNOGENICALLY DEPENDENT CONCENTRATIONS OF HEAVY METALS IN RIVER WATERS." LIFE OF THE EARTH 46, no. 4 (2024): 406–17. https://doi.org/10.29003/m4330.0514-7468.2020_46_4/406-417.

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Features of the prevalence of Cd and Pb dissolved forms in the water of sections of the Oka river and other rivers of the Russian Plain are considered. The influence of anthropogenic wastewater (industrial, municipal and agricultural) containing heavy metals is clearly manifested only in certain sections of the rivers of central Russia (Oka River, Volga River, and Moscow River) against the background of natural landscape and geochemical processes. An attempt is made to develop approaches to assessing the degree of anthropogenic influence on the water composition of various river sections, incl

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Zhu, Xianfu, Peiyu Li, Qingjie Gong, Weixuan Gu, Shengchao Xu, and Taotao Yan. "Geochemical Survey in Mojiang Area of Yunnan Province, China: Geochemical Map and Geochemical Anomaly Map." Applied Sciences 15, no. 5 (2025): 2592. https://doi.org/10.3390/app15052592.

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The geochemical maps and geochemical anomaly maps produced based on the data in the databases of the Regional Geochemistry–National Reconnaissance (RGNR) and the National Multipurpose Regional Geochemistry Survey (NMPRGS) projects have played a crucial role in China’s geochemical exploration. A geochemical survey of the Mojiang area, Yunnan Province, China, has been completed and reveals potential new regions for Ni exploration related to occurrences of serpentinite melanges. The geochemical maps and geochemical anomaly maps need to be drawn in this area. Traditional geochemical maps, heavily

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Rudykh, I. V. "Application of geochemical methods for direct prediction of hydrocarbon deposits in Western Yakutia." Vestnik of North-Eastern Federal University Series "Earth Sciences", no. 3 (September 21, 2023): 24–28. http://dx.doi.org/10.25587/svfu.2023.31.3.003.

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Based on the materials previously carried out by various types of geochemical surveys (water-gas, hydrochemical, litho-gas-geochemical, snow, atmochemical, bituminological sampling), an analysis of the oil and gas potential prospects of the eastern part of the Siberian platform within the Sakha Republic (Yakutia) established a direct relationship between the anomalies and the proven oil and gas potential of the studied territories. The indicators of geochemical field anomalies are an order of magnitude higher within territories with proven oil and gas potential (Nepa-Botuobinskaya anteclise) t

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Négrel, Philippe, Anna Ladenberger, Clemens Reimann, Manfred Birke, Alecos Demetriades, and Martiya Sadeghi. "GEMAS: Geochemical background and mineral potential of emerging tech-critical elements in Europe revealed from low-sampling density geochemical mapping." Applied Geochemistry 111 (December 2019): 104425. http://dx.doi.org/10.1016/j.apgeochem.2019.104425.

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Semina, I. S., and V. A. Androkhanov. "GEOCHEMICAL BACKGROUND IN SEMIMATURE SOILS MADE ON RECLAIMED SITES USING COAL WASTE." Ugol', no. 06 (June 8, 2022): 74–79. http://dx.doi.org/10.18796/0041-5790-2022-6-74-79.

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Arcanjo Paiola Ferreira, Daniela, Mariangela Garcia Praça Leite, Maria Cristina Teixeira Braga Messias, et al. "Spatial distribution and geochemical background of quartzitic and ferruginous rupestrian field soils." CATENA 246 (November 2024): 108369. http://dx.doi.org/10.1016/j.catena.2024.108369.

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Lavrusevich, A. A., I. M. Evgrafova, K. S. Polyakova, O. K. Vdovina, and R. V. Vysokinskaya. "Role of geochemical background at evaluation of investment attractiveness of recreational territories." Vestnik MGSU, no. 8 (August 2014): 98–106. http://dx.doi.org/10.22227/1997-0935.2014.8.98-106.

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Chen, Guoxiong, and Qiuming Cheng. "Fractal-Based Wavelet Filter for Separating Geophysical or Geochemical Anomalies from Background." Mathematical Geosciences 50, no. 3 (2017): 249–72. http://dx.doi.org/10.1007/s11004-017-9707-9.

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Hao, Libo, Xinyun Zhao, Yuyan Zhao, Jilong Lu, and Liji Sun. "Determination of the geochemical background and anomalies in areas with variable lithologies." Journal of Geochemical Exploration 139 (April 2014): 177–82. http://dx.doi.org/10.1016/j.gexplo.2013.11.007.

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Tsolova, Venera, Ivona Nikova, Biser Hristov, Kalin Ruskov, and Alexandar Zdravkov. "Geochemical patterns of soils in the Bobov dol valley, Bulgaria. Assessment of Cu, Pb and Zn contents." Bulgarian Journal of Soil Science 1, no. 2 (2016): 122–39. https://doi.org/10.5281/zenodo.2580816.

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The content of Si, Al, Fe, Ti, Mn, Mg, Ca, Na, K, S, P, C, Cu, Pb and Zn were determined in order to reveal geochemical patterns of soils in the Bobov dol valley, Bulgaria. Since the Bobov dol Thermal-electric Power Plant (TPP) is situated in the valley this paper pays attention to the geospatial distribution of Cu, Pb, and Zn due to their diverse vital significance. Elements assemblages and geospatial distribution pathways are also discussed in the light of the past 40 years of operation of the Thermal Power Plant. According to the results obtained the average content of Cu (27.04 mg kg-1 ),

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Andreev, D., and S. Buzmakov. "Anthropogenic transformation of forest ecosystems by geochemical and photosynthetic parameters." Anthropogenic Transformation of Nature 7, no. 2 (2021): 49–57. http://dx.doi.org/10.17072/2410-8553-2021-2-49-57.

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Geochemical and physiological indices gained at the background area and at the area under anthropogenic impact were compared. The study sites comprise 30 sample areas each. Overall, 600 samples of pine needles were designated for the delayed chlorophyll fluorescence measurement as well as 60 samples of soil and pine needle correspondingly were selected to perform the geochemical analysis. The biological uptake of the pine urban ecosystems is represented in the range: Mn (10,16) > P (7,19) > Ag (2,78) > Ba (2,76) > Cu (2,31) > Sr (1,85) > Ni (1,80) > Zn (1,75) > Pb (0,86

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Brotodewo, Adrienne, Caroline Tiddy, Diana Zivak, et al. "Recognising Mineral Deposits from Cover; A Case Study Using Zircon Chemistry in the Gawler Craton, South Australia." Minerals 11, no. 9 (2021): 916. http://dx.doi.org/10.3390/min11090916.

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Detrital zircon grains preserved within clasts and the matrix of a basal diamictite sequence directly overlying the Carrapateena IOCG deposit in the Gawler Craton, South Australia are shown here to preserve U–Pb ages and geochemical signatures that can be related to underlying mineralisation. The zircon geochemical signature is characterised by elevated heavy rare-earth element fractionation values (GdN/YbN ≥ 0.15) and high Eu ratios (Eu/Eu* ≥ 0.6). This geochemical signature has previously been recognised within zircon derived from within the Carrapateena orebody and can be used to distinguis

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