Relevant bibliographies by topics / Potential deposits

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
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Academic literature on the topic 'Potential deposits'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Potential deposits"

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Kontorovich, A. E., V. A. Kashirtsev, V. I. Moskvin, L. M. Burshtein, T. I. Zemskaya, E. A. Kostyreva, G. V. Kalmychkov, and O. M. Khlystov. "Petroleum potential of Baikal deposits." Russian Geology and Geophysics 48, no. 12 (December 2007): 1046–53. http://dx.doi.org/10.1016/j.rgg.2007.11.004.

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Yu, Fan, Qihai Shu, Xudong Niu, Kai Xing, Linlong Li, David R. Lentz, Qingwen Zeng, and Wenjie Yang. "Composition of Garnet from the Xianghualing Skarn Sn Deposit, South China: Its Petrogenetic Significance and Exploration Potential." Minerals 10, no. 5 (May 18, 2020): 456. http://dx.doi.org/10.3390/min10050456.

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The Xianghualing skarn Sn deposit in the southwestern part of the southern Hunan Metallogenic Belt is a large Sn deposit in the Nanling area. In this paper, the garnet has been analyzed by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) to obtain the concentrations of the major and trace elements. The results reveal that the garnets from the Xianghualing deposit mainly belong to andradite-grossular (grandite) solid solution and are typically richer in Al than in Fe. They show enrichment in heavy rare earth elements (HREEs) and notably lower light rare earth elements (LREEs), and commonly negative Eu anomalies, indicative of a relatively reduced formation environment. The garnets have high Sn concentrations between 2313 ppm and 5766 ppm. It is also evident that there is a positive correlation between Sn and Fe, suggesting that Sn4+ substitutes into the garnets through substituting for Fe3+ in the octahedral position. Combined with previous studies, it can be recognized that the Sn concentrations of garnet in skarn Sn deposits are generally high, whereas the W concentrations are relatively low. This is just the opposite in garnets from skarn W deposits that typically have high W, but low Sn concentrations. In polymetallic skarn deposits with both economic Sn and W, the concentrations of both metals in garnets are relatively high, although varying greatly. Therefore, the Sn and W concentrations in garnets can be used to evaluate a skarn deposit’s potential to produce Sn and (or) W mineralization, which is helpful in exploration.
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Mulanto, Tri. "Perilaku Konsumsi Upaya Meningkatkan Potensi Produk Deposito di Bank Syariah." Intizar 22, no. 2 (December 24, 2016): 333. http://dx.doi.org/10.19109/intizar.v22i2.945.

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Perbankan syari’ah saat ini telah memiliki payung hukum yang kuat dengan hadirnya undang-undang nomor 21 tahun 2008 tentang perbankan syari’ah. Hal ini sangat berpengaruh terhadap eksistensi dari perbankan syari’ah yang semakin diminati oleh banyak kalangan.Bank syari’ah membutuhkan dana dalam menjalankan produk pembiayaannya. Deposito merupakan salah satu produk penghimpunan di bank syariah. Deposito di bank syariah terus mengalami pertumbuhan. Walaupun demikian bank syariah tetap harus meningkatkan produk deposito, untuk mencapai market share 5 persen. Untuk meningkatkan volume deposito bank syariah perlu memahami bentuk perilaku konsumsi masyarakat. Dari data yang ada kontribusi dana pihak ketiga bank syariah diberikan oleh produk deposito sebesar 71,15 persen.Penulisan ini menggunakan jenis deskriptif kualitatif, Batasan dalam tulisan ini difokuskan pada produk deposito di bank syari’ah perilaku konsumen.Tulisan ini menggunakan studi pustaka kajian dari berbagai sumber. Hasil dari tulisan ini bahwa deposito di bank syariah terus mengalami perkembangan, pada tahun 2015 pertumbuhan deposito di bank syariah mencapai 4,12 persen. Perilaku konsumsi memiliki banyak faktor dan bisa memberi pengaruh terhadap peningkatan produk deposito di bank syariah. Sehingga bank syariah perlu memahami perilaku konsumsi masyarakat dalam upaya meningkatkan potensi pengembangan produk deposito di bank syariah.potensi pengembangan produk pembiayaan mudharabah di bank syari’ah masih sangat besar.Potensi pengembangan produk deposito masih sangat besar dan sangat luas.Bank of Shariah now has a solid legal with the presence of the law number 21 in 2008 about Bank of Shariah. This adversely affects the existence of the Shari'ah Bank that increasingly catches interest many people. Bank of Shari'ah requires funds in running financing products. Deposits are ones’ product accumulation in Islamic banks. Deposits in Islamic banks continued to grow. Nevertheless, Islamic banks still have to increase deposit products, to achieve a 5 percent market share. To increase the volume of deposits of Islamic banks need to understand the behaviors of consumption. From the available data the contribution of third party funds provided by the Islamic banks deposits amounted to 71.15 persen. This study uses a descriptive qualitative limitation. This paper is focused on products in Consumers Islamic bank deposits. This study uses literature review of various sources. The results of this paper that the deposits in Islamic banks continued to experienced growth, in 2015 the growth of deposits in Islamic banks reaches 4.12 percent. Consumer behavior has many factors and can give effect to an increase in deposit products in Islamic banks. So that Islamic banks need to understand the behavior of private consumption in order to increase the potential for product development of deposits in Bank of Shariah. The advantage of product development in Islamic bank financing is still enormous. The advantage of deposit product development is still very large and very spacious.
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Korandová, Beáta, Alena Straková, Jiří Beránek, and Dana Vrublová. "The raw material potential of the Czech Republic." Environmental Economics 9, no. 3 (October 8, 2018): 23–27. http://dx.doi.org/10.21511/ee.09(3).2018.03.

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This article summarizes the information on raw materials in the Czech Republic. Although mining was significantly reduced not long ago, there are still rich deposits of ores, non-metallic raw materials, as well as energetic and construction ones. Many of them are potentially utilizable in future, especially those which are economically favorable, and their mining is not in any conflict with environmental interests. Deposits are distributed irregularly, and their raw materials are different in both the Bohemian Massif and Western Carpathians. In order to be complete, the text also comprises deposits, which are restricted by environmental limits or their mining promises a low-cost effectiveness. The article is amended with actual statistical data.
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Hubarieva, Iryna, Olesіa Lebid, and Oleksandra Zuieva. "Determining the priority sources for attracting deposits in the formation of the financial potential of banks." Banks and Bank Systems 12, no. 3 (October 19, 2017): 215–27. http://dx.doi.org/10.21511/bbs.12(3-1).2017.06.

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The attraction of deposits by the banks in Ukraine is the basis for the formation of their resource base, which is an essential component of the banking financial potential. A qualitative formation of the bank’s resource base is carried out through proper management of attracting deposits in terms of their selection and giving preferences to specific sources of resource allocation. That is why the determination of priorities in attracting resources by banks and the formation of appropriate tools is an important tactical task in ensuring the stability of the Ukrainian banking system. The problem of new approaches to the management of deposits was especially acute during the crisis and the reduction of confidence of the population of Ukraine in the banking system, which makes actual the topic of the article and determines the importance of solving the tasks set in it. The goal of the paper is to develop tools for determining priorities of the main sources of attracting deposits by banks taking into account the system of criteria as a prerequisite for optimizing deposit portfolios of banks and the basis for the formation of their financial potential. The article proposes a sequence of stages and the corresponding tools that ensure the determination of priorities of different sources for attracting deposit funds of banks taking into account the criteria of time, minimization of costs and risks, balanced state of terms and volumes, equilibrium of costs and risks, ensuring a qualitative formation and effective use of the financial potential of the bank, ensuring a certain level of development of the bank. The use of the proposed approach made it possible to obtain such estimates that reflect priorities according to the criteria of minimization and equilibrium of risks and costs, a balanced state of terms and volumes and ensuring a specified level of the bank’s development, making it possible to determine the priorities of the main sources of attraction of financial resources for five banks in Ukraine.
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Ivanov, K. S., N. P. Kostrov, and V. A. Koroteev. "On the relationship of geodynamics, heat flow, deep structure and petroleum and gas potential of Yamal." Доклады Академии наук 486, no. 2 (May 27, 2019): 208–11. http://dx.doi.org/10.31857/s0869-56524862208-211.

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Hydrocarbon deposits concentration per unit square in Yamal is more than 100 times greater than the world average. Hydrocarbon deposits are generally located in regions with high modern geodynamic activity. The mantle structure in Yamal area has abnormal features according to seismic tomography. The southern part of Kara sea, Yamal and the western part of Gydan peninsula are situated in a big positive heat flow density anomaly with the epicenter near to Rusanovskoe deposit. Almost all deposits of hydrocarbones in Yamal are situated on the flanks of the West-Siberian rift system and simultaneously in gradient zones of heat flow density.
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Price, Gregory N. "The Cost of Government Deposits for Black-Owned Commercial Banks." Review of Black Political Economy 23, no. 1 (June 1994): 9–24. http://dx.doi.org/10.1007/bf02895738.

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This article utilizes a Statistical Cost Accounting Model and Mean Variance Model to estimate the cost and potential risk impact of government deposits for black-owned commercial banks. The main findings are that relative to other types of deposits on the balance sheet, government deposits are expensive, and that deposits received through the Minority Bank Deposit Program may have the effect of increasing risk in the asset portfolio.
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Pak, Sang-Joon, Inah Seo, Kyeong-Yong Lee, and Kiseong Hyeong. "Rare Earth Elements and Other Critical Metals in Deep Seabed Mineral Deposits: Composition and Implications for Resource Potential." Minerals 9, no. 1 (December 21, 2018): 3. http://dx.doi.org/10.3390/min9010003.

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The critical metal contents of four types of seabed mineral resources, including a deep-sea sediment deposit, are evaluated as potential rare earth element (REE) resources. The deep-sea resources have relatively low total rare earth oxide (TREO) contents, a narrow range of TREO grades (0.049–0.185%), and show characteristics that are consistent with those of land-based ion adsorption REE deposits. The relative REO distributions of the deep-seabed resources are also consistent with those of ion adsorption REE deposits on land. REEs that are not part of a crystal lattice of host minerals within deep-sea mineral deposits are favorable for mining, as there is no requirement for crushing and/or pulverizing during ore processing. Furthermore, low concentrations of Th and U reduce the risk of adverse environmental impacts. Despite the low TREO grades of the deep-seabed mineral deposits, a significant TREO yield from polymetallic nodules and REE-bearing deep-sea sediments from the Korean tenements has been estimated (1 Mt and 8 Mt, respectively). Compared with land-based REE deposits, deep-sea mineral deposits can be considered as low-grade mineral deposits with a large tonnage. The REEs and critical metals from deep-sea mineral deposits are important by-products and co-products of the main commodities (e.g., Co and Ni), and may increase the economic feasibility of their extraction.
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Nogueira, Grínia M., Cassiano Gomes Aimoli, Raquel Farias Weska, Leandro S. Nascimento, and Marisa Masumi Beppu. "In Vitro Calcification of Silk Fibroin Hydrogel." Key Engineering Materials 361-363 (November 2007): 503–6. http://dx.doi.org/10.4028/www.scientific.net/kem.361-363.503.

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Silk fibroin hydrogels were prepared and their potential to deposit calcium phosphates in vitro was observed. Pristine and lyophilized samples were tested in 1xSBF and 1.5xSBF. The results showed that silk fibroin hydrogels can induce calcium phosphate deposits both in the pristine and lyophilized form. However, the pristine silk fibroin hydrogel after calcification presented a fragile structure making it difficult to handle, while the lyophilized samples presented better resistance to handling. Calcium phosphates deposits were intense in samples submitted to tests in 1.5xSBF, however, few and isolated deposits were observed on samples submitted to tests in 1xSBF. The 3-D porous structure and the ability to deposit calcium phosphates, turn silk fibroin hydrogel a potential material suitable to use in biomimetic processes.
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Williams, K. J., S. J. Tait, and R. M. Ashley. "In-sewer sedimentation associated with active flow control." Water Science and Technology 60, no. 1 (July 1, 2009): 55–63. http://dx.doi.org/10.2166/wst.2009.286.

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Active flow control using automated gates and weirs aims to utilise available dispersed storage within sewer systems to alleviate the severity and frequency of localised flooding incidents. Whilst a previous study has demonstrated its potential, a key operational concern before implementation was sedimentation. An experimental programme was designed to investigate the sediment deposition created when using a flow control device. Tests were also undertaken to examine the potential for rapid gate opening to flush away any resulting deposits. In catchments dominated by fine material in suspension, the use of an active flow control device can result in a uniformly thick deposit upstream of the gate. Rapid gate opening results in deposited material eroding in large sections starting at the gate and moving in an upstream direction. Granular sediment forms a series of discrete bedforms which are fairly uniform regardless of the flow conditions and a larger deposit further upstream. The potential for flushing granular deposits is limited and modification of the operation of the gate has shown little potential for increasing the effectiveness. Therefore, active flow control using a single downstream gate may only be suitable in systems with fine material moving in suspension during dry weather flow and not where there is significant granular sediment.
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Dissertations / Theses on the topic "Potential deposits"

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John, Kangeze Biteme. "Ore forming potential of the Atchiza Suite and Sustainable management of mineral deposits in Mozambique : "Petrology, geochemistry and sustainable management of mineral deposits"." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-20380.

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Part 1- Abstract This research study presents detailed petrographic- and geochemical- analysis of 63 rock samples from the Atchiza Suite. The Suite is a layered mafic-ultramafic pluton located in the Tete Suite, of NW Mozambique. At present, the Atchiza comprises a group of three main types of rock that are classified based on their mineralogy, textures, geochemical composition. These are ultramafic cumulates (dunite and pyroxenites), mafic cumulates (medium-grained cumulate gabbro) and coarse-grained gabbro (non-cumulate gabbro). Compared to the rest of other rocks, coarse-grained gabbro shows high enrichment of Ti (0.64-3.46 wt% TiO2), Zr (5.9-296.1 5ppm), Sr (253.7-1268.4ppm) and V (224-952.3ppm), but relatively low depleted in compatible elements (Ni = 48.7-235.7ppm , Cr = below detection limit to 410.5ppm). Cumulate ultramafics are highly enriched in compatible elements (Ni up to 4636.2ppm, Cr up to 4721ppm). A high Mg# in ultramafic cumulates (0.59-0.86) suggests an Mg-rich primitive parental magma, whereas a low Mg# in coarse-grained gabbro (0.23-0.37) suggests a relatively high-differentiated magma. Cumulate gabbro shows Mg# ranging from 0.40-0.72, suggesting a moderately evolved magma source (derivative magma subsequent to fractionation of ultramafic cumulates). The Ni/Zr, Cr/Zr, Sr/Zr and Ti/Zr ratios are generally the lowest in coarse-grained gabbro when compared to cumulate rocks. The same applied; this suggests that coarse-grained gabbros were probably formed from a relatively high-differentiated magmatic liquid. In addition, the presence of an uninterrupted cryptic differentiation trend with these ratios implies that the Atchiza igneous lithologies were derived from one and the same parental melt. Apparently, Atchiza shows great variability of Fe2O3, SiO2 and SO3 during magmatic differentiation. There is significant decrease in Fe2O3, an increased SiO2 and SO3 contents in residual magma during progressive magma fractionation. It is true that all these geochemical changes will lower down the solubility of S in the system, thus providing a favourable condition for silicate-sulfide immiscibility. Theoretically, therefore, the Atchiza may have a potential to host Ni-Cu-(PGE) sulfide deposits. Part 2- Abstract Unlike water and forests, minerals are finite resources; they cannot be replaced back to their natural forms once they are depleted. For that reason, sustainable management of mineral resources is very important so that stakeholders in the extractive sector are guaranteed the same opportunities in sharing benefits. As part of this study, and with respect to Atchiza Suite, this section is discussing sustainable management of mineral deposits in Mozambique. Investment in Mozambican extractive industry should primarily be done with the main objective of poverty reduction for Mozambican citizens. Thus, the Mozambican Government needs to realize that proper management of mineral deposits will provide sufficient income for the country, enough to fund other development projects. Rather than being mismanaged, this massive collection of mineral revenues needs to be appropriately re-invested back to diversify other economic sectors. If this mineral revenue is managed wisely, the national annual budgets will be sufficiently supported. Most importantly, the country’s reliance on international loans and aids will be reduced significantly. Decision-making for development of the country’s mineral projects should not be central-governed; rather it should be transparent to the public and open for opinions and suggestions. As the main stakeholder in Mozambican extractive sector, local communities and civil societal groups should also be given opportunities to participate in decision-making, important for the development of mining projects. Mineral agreements for which the Mozambican State has been signing with multinational companies for development of the country’s mineral projects need to be published and be available publicly. In addition, negotiation of mining agreements must be transparent and involve all stakeholders. Investment and development of the country’s mineral projects must be performed through partnerships and Joint ventures between multinational mining companies, national-based companies and the Mozambican State. Development of mineral deposits must incorporate environmental sustainability. Despite its high mineral potential (e.g. Ni-Cu-PGE-Ti-V), Atchiza also is surrounded by a wide range of other natural resources. The Cahora Bassa Dam, which is located just adjacent to Atchiza Project, is the main source of clean energy not only for Mozambique domestic market, but also for the majority of Sub-Saharan countries. All of these natural resources require good practice of Environmental sustainability in mining activities.
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Sulaeman, Hanif Ibadurrahman. "Discovery of Paleotsunami Deposits along Eastern Sunda Arc: Potential for Megathrust Earthquakes in Bali." BYU ScholarsArchive, 2018. https://scholarsarchive.byu.edu/etd/7178.

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Several laterally extensive candidate tsunami deposits are preserved along coastlines facing the eastern Java Trench, indicating it has experienced mega-thrust earthquakes in the past. We investigated 37 coastal sites in Bali, Lombok, Sumba and Timor islands, many of which preserve course sand and pebble layers that overlie sharp basal contacts with scour marks into the mud, fine upward in grain size, and have bimodal grain size distributions. Other unique features are the common occurrence of marine fossils and concentrations of heavy minerals. The occurrence of these high-energy deposits interlayered with clay-rich units indicates the coarse clastics are anomalous because they were deposited in what is normally a very low-energy depositional environment. The lateral extent and paucity of thin, coarse clastic layers with marine organisms are inconsistent with local stream flood event, and the proximity to the equator of the sites diminishes the possibility of marine flood events from cyclones. The sparse, but consistent, the occurrence of at least two candidate tsunami deposits at depths of 1 and 2 meters over 950 km along the strike of the Java Trench may reveal that mega-thrust earthquakes have occurred there and generated giant tsunamis in the recent past. Five widely scattered imbricated boulder deposits are also found on Bali, Lombok, and Sumba. The boulders consist of slabs of hardpan up to 2.5 m in length and 80 cm thick that was torn from a near-shore seabed and stacked on top of one another. Some of the boulders were carried over the erosional coastal bank and deposited up to 100 meters inland. Comparisons with imbricated boulder ridges formed during the 1994 tsunami in east Java indicate that these deposits are from one or multiple tsunamis sourced by the Java Trench. Experiments in effective ways to communicate and implement tsunami disaster mitigation strategies have led us to train local communities about the 20-20-20 rule. If coastal communities experience more than 20 seconds of shaking from an earthquake, even if it is not intense, they should evacuate the coast. The time delay between the earthquake and arrival of tsunami waves is around 20 minutes, which is the time window for evacuation. Some tsunami waves may be as high as 20 meters, which is the target elevation for evacuation. Adopting the 20-20-20 rule could save thousands of lives throughout the region, especially in Bali where nearly 1 million people inhabit likely tsunami inundation zones.
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Michnowicz, Sabina Anna Katarzyna. "Exploratory study of the potential airborne health hazard of dusts generated by quarrying volcanic deposits." Thesis, Durham University, 2014. http://etheses.dur.ac.uk/10919/.

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Occupational exposure to dust generated by quarrying siliceous rocks (i.e. sandstone, coal) is a well documented respiratory hazard. Hazard of volcanic ash inhalation is also routinely studied (although less well understood), but the specific respiratory hazard of quarried volcanic deposits is entirely under-researched and is the focus of this study. The two main factors potentially implicated in respiratory toxicity of volcanic quarry dust are: i) crystalline silica content implicated in silicosis and lung cancer; and ii) iron-catalysed hydroxyl radical generation, implicated in inflammation and carcinogenesis. Twelve sites (in New Zealand, Montserrat and Greece), quarrying a range of volcanic deposits, were investigated and compared with volcanic ash samples (to test suitability as an analogue) and dust from non-volcanic quarries (greywacke and sandstone) in an investigation of the physicochemical characteristics which may influence particle surface reactivity. Samples of deposited dust (<1mm size fraction) were collected and 11 of these separated to ≤10μm for further analyses. Compositional analyses (XRF) showed the samples spanned the range of magmatic compositions from mafic to felsic (44-76 wt.% SiO2). The finest material was generated by drilling lava flows (8.3-27.5 cu.vol% <10 μm diameter particles in <1mm fraction), however, several other sample types (i.e. dust on processor) contained high levels of respirable material, akin to volcanic ash from equivalent eruption settings. SEM analyses confirmed particles to be blocky and angular, having aspect ratios between 0.59-0.70 (<10μm fraction). Crystalline silica content was highest (up to 28 wt. %) in dusts from intermediate and felsic quarries where lava domes (or collapse deposits) are mined. Similar levels were observed for dome-collapse ash and greywacke quarry dusts; however, the sandstone quarry dust was 99 wt.% crystalline silica. Hydroxyl radical generation was lower for quarried volcanic samples than for either volcanic ash or sandstone (significant to p≤0.01 for mafic ash/quarry dust). Haemolysis (erythrocyte membrane rupture, an indicator of quartz reactivity) was exhibited by six samples from three quarries, and comparable to the DQ12 quartz positive standard, when adjusted for surface area. These findings may be influenced by the presence of clays, however, as haemolytic samples included those with little crystalline silica. Airborne dust levels (both role-specific and ambient) were measured in the quarries and were mostly within international exposure limits, however, interpretations were limited by the duration of measurements so further work is required. Some workers’ shifts were longer than 8 hours, and workers on Montserrat may also be simultaneously exposed to volcanic ashfall, which should be considered with respect to adherence to regulations in those quarries. Mitigation measures were variable and workers would benefit from better awareness regarding use of non-mandatory respiratory protection. Volcanic quarries pose a hazard distinct from volcanic ash and from non-volcanic quarries. Overall, hazard may be lower than for quarrying other rock types, but further research is needed to better constrain the potential hazards. Until then, a precautionary approach might be taken in quarries where respirable dust levels are high and deposits may contain crystalline silica or iron.
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Malehmir, Alireza. "3D Geophysical and Geological Modeling in the Skellefte District: Implications for Targeting Ore Deposits." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-8188.

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With the advancements in acquisition and processing of seismic reflection data recorded over crystalline rocks, building three-dimensional geologic models becomes increasingly favorable. Because of little available petrophysical data, interpretations of seismic reflection data in hardrock terrains are often speculative. Potential field data modeling are sometimes performed in order to reduce the ambiguity of seismic reflection interpretations. The Kristineberg mining area in the western part of the Paleoproterozoic Skellefte Ore District was chosen to construct a pilot three-dimensional geologic model in an attempt to understand the crustal architecture in the region and how the major mineral systems operated in this architecture. To contribute to this aim, two parallel seismic reflection profiles were acquired in 2003 and processed to 20 sec with special attention to the top 4 sec of data. Several reflections were imaged and interpreted by the aid of reflector modeling, borehole data, 2.5D and 3D potential field modeling, and geological observations. Interpretations are informative at the crustal scale and help to construct a three-dimensional geologic model of the Kristineberg mining area. The three-dimensional geologic model covers an area of 30×30 km2 down to a depth of 12 km. The integrations help to interpret a structural basement to the Skellefte volcanic rocks, possibly with Bothnian Basin metasedimentary affinity. The contact is a shear-zone that separates the two units, generating large fold structures, which can be observed in the region. The interpretations help to divide the Revsund granitic rocks into two major groups based on their present shape and thickness. A large gravity low in the south is best represented by the intrusion of thick dome of Revsund granite. In the north, the low-gravity corresponds to the intrusion of sheet-like Revsund granites. In general, the structure associated with the Skellefte volcanics and the overlying metasedimentary rocks are two thrusts exposing the Skellefte volcanic rocks in the cores of hanging wall anticlinal structures. Lack of coherent reflectivity in the seismic reflection data may be due to complex faulting and folding systems observed in the Skellefte volcanics. Ultramafic sills within the metasedimentary rocks are interpreted to extend down to depths of about 5-6 km. The interpretations are helpful for targeting new VHMS deposits and areas with gold potential. For VHMS deposits, these are situated in the southern limb of a local synformal structure south of the Kristineberg mine, on the contact between the Revsund granite and the Skellefte volcanic rocks. A combination of metasedimentary and mafic-ultramafic rocks are highly gold prospective in the west, similar to observations elsewhere in the region. There are still questions that remain unanswered and need more work. New data in the study area will help to answer questions related to e.g., an enigmatic diffraction seismic signal in Profile 5 and the structural relationship between the Skellefte volcanic rocks and the Malå volcanics. Although the derived 3D geologic model is preliminary and constructed at the crustal scale, it provides useful information to better understand the tectonic evolution of the Kristineberg mining area.

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Makhubele, Marvel M. H. "The role of salt tectonics in the hydrocarbon potential of the post-salt deposits (Albian to Recent), offshore Gabon." Thesis, University of Western Cape, 2014. http://hdl.handle.net/11394/3497.

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Magister Scientiae - MSc
Following successful discovery and production of hydrocarbons, Gabon is one of the key hydrocarbon target countries in Africa. Located in the Lower Congo Basin, the study area is based in Etame Marin Permit (EMP), which is licensed to VAALCO Energy Inc., and has been producing hydrocarbons since 2002. The currently explored and producing reservoirs are in the pre-salt sandstones of the Aptian Gamba Formation, charged with hydrocarbons sourced from the syn-rift lacustrine shale of the pre-Aptian Melania Formation. With the aim of finding potential petroleum plays in the post-salt successions and by using 3D prestack depth migration (PSDM) seismic sections and wireline logs, a detailed study of the post-Aptian stratigraphy and salt tectonics of the EMP was undertaken. Eight distinct reflectors were identified based on gamma ray signatures, stratal terminations and isopach trends. Sediment distribution patterns and the relative sea level history of the succession were determined by applying principles of sequence stratigraphy and salt tectonics. Furthermore, two potential plays have been outlined in the post-salt carbonates of the Albian Madiela Formation as well as in sandstones of the Turonian Azile Formation. These reservoirs might have been charged with hydrocarbons from the pre-salt shale of the Melania Formation and/or potentially also enriched from the Albian and Cenomanian shales. For these post-salt hydrocarbon reservoirs to be charged by the pre-salt source rocks, windows within the extensive evaporitic sealing of the Aptian Ezanga Formation were required. 3D PSDM seismic sections attest that diapirism of the Aptian salt unit generated ample hydrocarbon migration pathways from the pre-salt source rocks to post-salt reservoirs. Five well-developed potential salt windows have been identified, two of which have good probability to have facilitated the upward migration of hydrocarbons, because these salt windows are located up dip of oil producing wells. However, even if hydrocarbons are found in the post-salt reservoirs, similarly to the Yombo Field (located offshore Congo, south of the EMP), these shallow reservoirs in the EMP are likely to produce heavy oils due to biodegradation.
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Weatherington-Rice, Julie Bishop Paynter. "Fracture occurrence and ground water pollution potential in Ohio's glacial and lacustrine deposits: a soils, geologic, and educational perspective." The Ohio State University, 2003. http://rave.ohiolink.edu/etdc/view?acc_num=osu1072118096.

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Reardon, Timothy W. "Modern Marine Sediments of Bahia Concepcion : Patterns, Processes, and Potential Analogues to Neogene Rift Basin deposits of Baja California." Oberlin College Honors Theses / OhioLINK, 1995. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1411645561.

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Akçay, Migraç. "Genesis of the stibnite-cinnabar-scheelite deposits of the Gumusler area, Nigde, central Turkey and implications on their gold potential." Thesis, University of Leicester, 1994. http://hdl.handle.net/2381/34995.

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The project aims to describe the geology and hydrothermal fluid evolution of mineral deposits of the Gumusler area in the Nigde massif. Two types of deposits can be differentiated in this area: Sb Hg W Ba Au veins and associated replacement type Ba- Sb mineralization at the Rasih-Ihsan deposit, and a breccia hosted Hg Sb Au prospect at the Mehmetler Yurdu Sivrisi Tepe (MYST). The vein deposits are localized along E-W trending and N-dipping faults in marbles, and along marble-gneiss contacts. There is a spatial relationship between the mineral deposits and the felsic dykes of Cenomanian age which are cut by tlie Sb-Hg- W Ba vein. Similar dykes, together with intensive fracturing of marbles along the gneiss- marble contacts, also contributed to the formation of approximately E-W trending breccias containing the Hg Sb Au prospect at the MYST area. The Gumusler deposits have a diverse mineralogy including scheelite, barite, stibnite, cinnabar, sulphosalts and gold. Gold is associated with the cinnabar deposition stage, and is locally enriched in near surface zones with concentrations as high as 37 ppm at the MYST prospect. Silicification is the dominant wall rock alteration at the mineralized locations but sericitization, kaolinization, dolomitization and tourmalinization also occur at the periphery of the mineralization. Mineral deposition took place from aqueous fluids over a wide temperature range ( 350 °C to 150 °C). The pre-sulphide alteration (tourmalinization) occurred from fairly saline (8 2.5 eq. wt % NaCl) and moderately high temperature (216-254 °C) fluids. The main barite deposition also took place from fairly saline (8 2.5 eq. wt % NaCl) fluids at temperatures of 149-213 °C which are diluted towards the stibnite stage with a salinity of 4 eq. wt % NaCl and a temperature range of 137-168 °C. This probably indicates increasing involvement of non-magmatic waters. delta34S values of pyrite and stibnite range from -4.3 to +2.2 ‰ whereas those of barite are ~18 %, which suggests a magmatic origin for the sulphur of both sulphide and sulphate. Tourmaline mineral chemistry of hydrothermal alteration zones indicates a mixture of granitic and metapelitic sources, but comparison with tourmalines of other magmatic deposits favours a magmatic origin for boron.
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Minde, Peder. "Clast analysis of potential resurge deposits as part of the Vakkejokk Breccia in the Torneträsk area, northern Sweden - a proposed impact ejecta layer." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-143782.

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In the northern part of Swedish Caledonides, north of Lake Torneträsk is a 7 km long exposure of a breccia layer. The layer thins westwards and eastwards from the central part where it is up to 27 m thick. It is called the Vakkejokk Breccia after the type section. The breccia has been described in literature since about a century, but its origin is enigmatic. The breccia layer is since the summer of 2012 investigated by three geologists specialized in impact craters, Paleozoic sediments, and the Caledonian orogeny. They put forward evidence for the breccia being formed by a hypervelocity impact during the Lower Cambrian at approximately 520 Ma (Ormö et al. 2017). At that time the target area was a shallow epicontinental sea that surrounded the mainly peneplanized continent Baltica. An impact into the sea is known to generate tsunami waves as well as resurge deposits when the water brings ejected and rip-up material back into the crater. Ormö et al. (2017) suggest the top part of the Vakkejokk Breccia to include such resurge deposits. The depositional marine environment is also known to rapidly protect an impact crater from further erosion. It is possible that only the topographic rim of the Vakkejokk crater was eroded during the millions of years it may have taken before the crater was covered by younger sediments. About 100 m.y. after the formation, it was completely covered by overthrust nappes during the Caledonian orogeny, when Baltica and Laurentia collided. The crater itself is not exposed today, merely parts of what is thought to be the ejecta layer and resurge deposits. This Bachelor of Science project aimed to investigate the putative resurge deposits to learn more about the process of formation and the provenance in the target of the clasts in the deposits. This was carried out by three short drillcores through the resurge deposit part of the Vakkejokk Breccia layer. The place to drill the boreholes was chosen at an outcrop which is proximal to the putative hidden crater. The retrieved drillcores were cut longitudinally, then polished and photographed in high resolution. Each core was then analyzed in an image analysis software with respect to clast granulometry and lithology. To the results are presented as graphs showing clast size, size sorting, clast shape, of the relative amounts of different lithologies and the matrix content. The results are discussed with respect to well-documented analogue marine-target craters
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Dwairi, I. M. A. "A chemical study of the palagonitic tuffs of the Aritain area of Jordan, with special reference to nature, origin and industrial potential of the associated zeolite deposits." Thesis, University of Hull, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.233955.

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Books on the topic "Potential deposits"

1

Gray, Jerry J. Bentonite in Oregon: Occurrences, analyses, and economic potential. Portland, Or: State of Oregon, Dept. of Geology and Mineral Industries, 1989.

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McArdle, Peadar. Rare earths in Ireland: The potential for deposits. Dublin: Geological Survey of Ireland, 1987.

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Hahn, Lothar. Outline of the geology and the mineral potential of Thailand. Hannover: Bundesanstalt für Geowissenschaften und Rohstoffe und den geologischen Landesämtern in der Bundersrepublik Deutschland, 1986.

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Gunther, Thomas. The potential supply of minerals from undiscovered copper-silver deposits in the Kootenai National Forest. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1990.

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Gunther, Thomas. The potential supply of minerals from undiscovered copper-silver deposits in the Kootenai National Forest. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1990.

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Gunther, Thomas. The potential supply of minerals from undiscovered copper-silver deposits in the Kootenai National Forest. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1990.

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Schwochow, S. D. Geology and resource potential of strategic minerals in Colorado. Denver, Colo: Colorado Geological Survey, Dept. of Natural Resources, State of Colorado, 1985.

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Gray, Jerry J. Bentonite in Oregon: Occurrences, analyses, and economic potential / by Jerry J. Gray, Ronald P. Geitgey, and Gary L. Baxter. Portland, Or: Dept. of Geology and Mineral Industries, 1989.

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Malik, Rashid Hussain. Geology and resource potential of Kashmir rugy deposits, Distt. Muzaffarabad (AK) Pakistan. Muzaffarabad, Azad Kashmir: Azad Kashmir Mineral and Industrial Development Corp., 1994.

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Budhu, M. Liquefaction potential of surficial deposits in the city of Buffalo, New York. Buffalo, N.Y: National Center for Earthquake Engineering Research, 1989.

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Book chapters on the topic "Potential deposits"

1

Schwarz-Schampera, Ulrich. "The Potential of Thorium Deposits." In Uranium, Mining and Hydrogeology, 53–58. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_7.

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Luodes, Hannu, Heikki Sutinen, Paavo Härmä, Heikki Pirinen, and Olavi Selonen. "Assessment of Potential Natural Stone Deposits." In Engineering Geology for Society and Territory - Volume 5, 243–46. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_47.

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Lydon, John W. "The Potential for Hydrothermal Platinum Deposits." In Geo-Platinum 87, 111–12. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-1353-0_11.

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Elitok, Ömer, and Metin Tavlan. "Geology and Economic Potential of Ni Deposits." In Modern Approaches in Solid Earth Sciences, 635–53. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-02950-0_13.

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Obando, Luis Gmo, Luis R. Malavassi, and Rodrigo Estrada. "Deposits of Peat in Costa Rica." In Energy and Mineral Potential of the Central American-Caribbean Region, 199–207. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-79476-6_27.

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Parnell, J. "Metal Enrichments in Bitumens from the Carboniferous of Ireland: Potential in Exploration for Ore Deposits." In Bitumens in Ore Deposits, 475–89. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85806-2_26.

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Grossou-Valta, M., K. Adam, D. C. Constantinides, J. M. Prevosteau, and E. Dimou. "Mineralogy of and potential beneficiation process for the Molai complex sulphide orebody, Greece." In Sulphide deposits—their origin and processing, 119–33. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0809-3_8.

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Cohen, Arthur D., Oldemar Ramirez, Luis Obando, Luis Malavassi, and Arturo Ramirez. "Peat Deposits of Central America and the Caribbean Region." In Energy and Mineral Potential of the Central American-Caribbean Region, 193–97. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-79476-6_26.

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Meng, Choong Chee, Nur Huda M. Jamin, Muhammad Azfar Mohamed, and Chin Soon Mun. "Sedimentology of Potential Tertiary Fluvial Deposits in Kluang, Johor, Malaysia." In ICIPEG 2016, 313–21. Singapore: Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-3650-7_27.

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Ritchey, Joseph L., Nicholas Wetzel, Scott A. Stebbins, and Benjamin W. Haynes. "Economic Perspective on Development of Potential Gorda Ridge Sulfide Deposits." In Gorda Ridge, 143–52. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4612-3258-2_9.

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Conference papers on the topic "Potential deposits"

1

Caprotti, Rinaldo, Angela Breakspear, Olaf Graupner, Thomas Klaua, and Oliver Kohnen. "Diesel Injector Deposits Potential in Future Fueling Systems." In Powertrain & Fluid Systems Conference and Exhibition. 400 Commonwealth Drive, Warrendale, PA, United States: SAE International, 2006. http://dx.doi.org/10.4271/2006-01-3359.

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Chernov, A. A., and V. A. Boldyreva. "The Estimation of Paleozoic Deposits Potential in Predkavkazye." In Saint Petersburg 2008. Netherlands: EAGE Publications BV, 2008. http://dx.doi.org/10.3997/2214-4609.20146933.

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M. Grechneva, O., G. L. Rozbaeva, and A. A. Nateganov. "Petroleum Potential of Russko-Rechenskoye Low-Cretaceous Deposits." In 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20149574.

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Baldin, V. A. "Hydrocarbon Potential of Riphean-paleozoic Deposits of Taimyr." In Saint Petersburg 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143597.

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Stanton, Kelsay M., and Juliet Crider. "DIFFERENTIATING QUATERNARY ESTUARINE DEPOSITS FROM POTENTIAL PRE-LATE WISCONSIN OUTWASH DEPOSITS SOUTHWESTERN WASHINGTON COAST." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-354286.

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Slack, John F. "METALLIC MINERAL DEPOSITS OF NEW ENGLAND: HISTORICAL OVERVIEW, KNOWN DEPOSITS, AND POTENTIAL UNDISCOVERED RESOURCES." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-327914.

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Greig-Jones, Shelly-Ann, Jill K. Marcelle-de Silva, and Sydney Thomas. "Resource Potential of Natural Gas Hydrate Deposits Offshore Trinidad." In SPETT 2012 Energy Conference and Exhibition. Society of Petroleum Engineers, 2012. http://dx.doi.org/10.2118/158542-ms.

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Ranasinghe, D. Y. L., H. M. S. Lakmal, H. M. H. K. Weerasooriya, E. M. M. B. Ekanayake, G. M. R. I. Godaliyadda, H. M. V. R. Herath, and M. P. B. Ekanayake. "Hyperspectral Imaging Based Method to Identify Potential Limestone Deposits." In 2019 IEEE 14th Conference on Industrial and Information Systems (ICIIS). IEEE, 2019. http://dx.doi.org/10.1109/iciis47346.2019.9063280.

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Fourie, Andries. "Liquefaction Potential of Surface Deposits of High-Density Thickened Tailings." In Ninth International Seminar on Paste and Thickened Tailings. Australian Centre for Geomechanics, Perth, 2006. http://dx.doi.org/10.36487/acg_repo/663_10.

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Zhang, Y. N., X. Cao, and P. Wanjara. "Fiber Laser Deposition of Nickel-Based Superalloys Using Filler Wire Feed." In ASME Turbo Expo 2015: Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/gt2015-42055.

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In this work, a continuous wave fiber laser welding system was used to deposit nickel-based superalloys Inconel 718 (IN 718) and Waspaloy using filler wire feed sources. The multi-bead and multi-layer deposits that were manufactured were characterized in terms of the macro- and microstructures, defects, and hardness in both the as-deposited and fully heat treated conditions. The tensile properties of the deposits in the heat treated condition were also determined and compared to the existing aerospace materials specifications. Using optimized laser processing parameters, high strength deposits could be manufactured, though minor weld metal liquation cracking for IN718 and strain-age cracking for Waspaloy were present, which compromised slightly the ductility as compared to wrought aerospace specifications for the two alloys. The successful development of the direct laser deposition process using wire feeding indicates the potential of employing the fiber laser technology to manufacture nickel-based superalloy aerospace components.
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Reports on the topic "Potential deposits"

1

Bell, R. T., and S. S. Gandhi. Olympic Dam - Type Deposits: Potential in Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131191.

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Paradis, S. Carbonate-hosted Zn-Pb deposits in southern British Columbia - potential for Irish-type deposits. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/224161.

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Poulin, R. S., A. M. McDonald, D. J. Kontak, and M. B. McClenaghan. Scheelite geochemical signatures and potential for fingerprinting ore deposits. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296473.

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Poulsen, K. H. Carlin-type gold deposits and their potential occurrence in the Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207403.

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Kjarsgaard, B. A. Potential for rare earth and rare metal deposits, Thaidene Nene MERA study area. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292462.

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Georgieva, Sylvina, Elitsa Stefanova, Atanas Hikov, and Irena Peytcheva. Trace Element Geochemistry of Alunite from the Chelopech High-sulphidation Epithermal Deposit, Bulgaria: a Potential Tool for Exploration of Epithermal Deposits. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, August 2020. http://dx.doi.org/10.7546/crabs.2020.08.07.

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Gandhi, S. S., and J. A. Kerswill. Potential for Mississippi Valley-type lead-zinc deposits in the Artillery Lake area, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292467.

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Witherly, K. E. Application of applied potential and downhole pulse EM techniques to exploration for massive sulphide deposits in eastern Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/123637.

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Dulfer, H., R. G. Skirrow, D. C. Champion, L. M. Highet, K. Czarnota, R. Coghlan, and P. R. Milligan. Potential for intrusion-hosted Ni-Cu-PGE sulfide deposits in Australia: A continental-scale analysis of mineral system prospectivity. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.001.

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Huntley, D. H., and A. S. Hickin. Surficial deposits, landforms, glacial history and potential for granular aggregate and frac sand: Maxhamish Lake map sheet (NTS 94O), British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/261697.

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