Relevant bibliographies by topics / Calderas Geology Geology, Economic

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Calderas Geology Geology, Economic'

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Published: 4 June 2021
Last updated: 3 February 2022

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Journal articles on the topic "Calderas Geology Geology, Economic"

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Mueller, W. U., J. Stix, P. L. Corcoran, and R. Daigneault. "Subaqueous calderas in the Archean Abitibi greenstone belt: An overview and new ideas." Ore Geology Reviews 35, no. 1 (March 2009): 4–46. http://dx.doi.org/10.1016/j.oregeorev.2008.12.003.

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Rosera, Joshua M., Sean P. Gaynor, and Drew S. Coleman. "Spatio-Temporal Shifts in Magmatism and Mineralization in Northern Colorado Beginning in the Late Eocene." Economic Geology 116, no. 4 (June 1, 2021): 987–1010. http://dx.doi.org/10.5382/econgeo.4815.

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Abstract Magmatism in northern Colorado beginning in the late Eocene is associated with the formation of Pb-Zn-Ag carbonate-replacement and polymetallic vein deposits, the onset of caldera-forming magmatism, and eventually, the formation of rift-related, F-rich Mo porphyries (“Climax-type” intrusions). We use high-precision U/Pb zircon geochronology to better evaluate the temporal framework of magmatism and mineralization in the region. Our results demonstrate that mineralization in the Leadville area occurred between 43.5 and 39.7 Ma and was followed by mesothermal mineralization in the Montezuma area at approximately 38.7 Ma. Mineralization is associated with a suite of approximately 43 to 39 Ma intermediate magmatic centers that extended from Twin Lakes through Montezuma. The oldest porphyries associated with F-rich Mo prospects and deposits (Middle Mountain; 36.45 Ma) intruded 900 kyr after the start of the ignimbrite flare-up in the region. Spatiotemporal analyses reveal that the pattern of magmatism shifted in orientation between 40 and 35 Ma. We propose a model wherein magmatism before 39 Ma was the result of fluids evolved from the subducted Farallon slab being focused through weak zones in the lithospheric mantle and into the lower crust. This was followed by a more diffuse and higher power melting event that corresponds to a distinct change in the spatial patterns of magmatism. Our data suggest that low-grade Mo porphyry deposits can form close in time to calderas. We hypothesize that the transition from subduction to extensional tectonics in the region was responsible for this more widespread melting and a distinct shift in the style of magmatic-hydrothermal mineralization.
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Hwang, Sang Koo, Young Woo Son, Seung Hwan Seo, and Weon-Seo Kee. "Collapse Type and Processes of the Geumosan Caldera in the Southern Gumi, Korea." Economic and Environmental Geology 54, no. 1 (February 28, 2021): 35–48. http://dx.doi.org/10.9719/eeg.2021.54.1.35.

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Keith, Manuel, Karsten M. Haase, Florian Häckel, Ulrich Schwarz-Schampera, Reiner Klemd, Mark Hannington, Harald Strauss, Timothy McConachy, and Melissa Anderson. "Trace element fractionation and precipitation in submarine back-arc hydrothermal systems, Nifonea caldera, New Hebrides subduction zone." Ore Geology Reviews 135 (August 2021): 104211. http://dx.doi.org/10.1016/j.oregeorev.2021.104211.

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Mauri, Guillaume, Alwi Husein, Adriano Mazzini, Karyono Karyono, Anne Obermann, Guillaume Bertrand, Matteo Lupi, Hardi Prasetyo, Soffian Hadi, and Stephen A. Miller. "Constraints on density changes in the funnel-shaped caldera inferred from gravity monitoring of the Lusi mud eruption." Marine and Petroleum Geology 90 (February 2018): 91–103. http://dx.doi.org/10.1016/j.marpetgeo.2017.06.030.

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Johnston, David, Brad Scott, Bruce Houghton, Douglas Paton, David Dowrick, Pilar Villamor, and John Savage. "Social and economic consequences of historic caldera unrest at the Taupo volcano, New Zealand and the management of future episodes of unrest." Bulletin of the New Zealand Society for Earthquake Engineering 35, no. 4 (December 31, 2002): 215–30. http://dx.doi.org/10.5459/bnzsee.35.4.215-230.

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In 1998, changes in a number of indicators (earthquakes and uplift) at two of New Zealand's active volcanic caldera systems (Okataina and Taupo) resulted in increased public, local and central government awareness and some concern about the potential significance of volcanic unrest at a caldera volcano. This paper summarises the episodes of unrest recorded at Taupo caldera since 1895. There have been four significant events (1895, 1922, 1963-64 and 1983) that have included earthquake activity and ground deformation. Caldera unrest is one of the most difficult situations the volcanological and emergency management communities will have to deal with. There is potential for adverse social and economic impacts to escalate unnecessarily, unless the event is managed appropriately. Adverse response to caldera unrest may take the form of the release of inappropriate advice, media speculation, unwarranted emergency declarations and premature cessation of economic activity and community services. A non-volcanic-crisis time provides the best opportunity to develop an understanding of the caldera unrest phenomena, and the best time to establish educational programmes, funding systems for enhanced emergency response and volcano surveillance and to develop co-ordinated contingency plans.
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YOKOYAMA, Hikaru, Masahiro YAHATA, Satoshi OKAMURA, and Hirotsugu NISHIDO. "Volcano-stratigraphy and geological development of Akaigawa Caldera from southwest Hokkaido, Japan." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 2 (2003): 80–95. http://dx.doi.org/10.2465/gkk.32.80.

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Rytuba, James J., Raul J. Madrid, and E. H. McKee. "Relationship of the Cortez Caldera to the Cortez Disseminated Gold Deposit, Nevada." Journal of Geochemical Exploration 25, no. 1-2 (March 1986): 251. http://dx.doi.org/10.1016/0375-6742(86)90046-4.

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Holmes, D. C., A. E. Pitty, and D. J. Noy. "Geomorphological and hydrogeological features of the Poços de Caldas caldera analogue study sites." Journal of Geochemical Exploration 45, no. 1-3 (November 1992): 215–47. http://dx.doi.org/10.1016/0375-6742(92)90126-s.

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Somma, Renato, Daniela Blessent, Jasmin Raymond, Madeline Constance, Lucy Cotton, Giuseppe De Natale, Alessandro Fedele, et al. "Review of Recent Drilling Projects in Unconventional Geothermal Resources at Campi Flegrei Caldera, Cornubian Batholith, and Williston Sedimentary Basin." Energies 14, no. 11 (June 4, 2021): 3306. http://dx.doi.org/10.3390/en14113306.

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Unconventional geothermal resource development can contribute to increase power generation from renewable energy sources in countries without conventional hydrothermal reservoirs, which are usually associated with magmatic activity and extensional faulting, as well as to expand the generation in those regions where conventional resources are already used. Three recent drilling experiences focused on the characterization of unconventional resources are described and compared: the Campi Flegrei Deep Drilling Project (CFDDP) in Italy, the United Downs Deep Geothermal Power (UDDGP) project in the United Kingdom, and the DEEP Earth Energy Production in Canada. The main aspects of each project are described (geology, drilling, data collection, communication strategies) and compared to discuss challenges encountered at the tree sites considered, including a scientific drilling project (CFDDP) and two industrial ones (UDDGP and DEEP). The first project, at the first stage of pilot hole, although not reaching deep supercritical targets, showed extremely high, very rare thermal gradients even at shallow depths. Although each project has its own history, as well as social and economic context, the lessons learned at each drilling site can be used to further facilitate geothermal energy development.
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Dissertations / Theses on the topic "Calderas Geology Geology, Economic"

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Immitt, James Peter. "Mineralización tipo skarn y vetas epitermales en la región de la Caldera de San Carlos, noreste de Chihuahua." Mexico, D.F. : Ciudad Universitaria, 1987. http://catalog.hathitrust.org/api/volumes/oclc/21342689.html.

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Thesis (M.A.)--University of Texas at Austin, 1981.
Three maps on 3 folded leaves in pocket. Summary in English. Translation of: Skarn and epithermal vein mineralization in the San Carlos Caldera region, northeastern Chihuahua, Mexico. Includes bibliographical references (p. 63-66).
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Kennedy, Ben. "Magmatic processes associated with the development of large silicic calderas." Thesis, McGill University, 2005. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=100637.

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Large caldera-forming eruptions are among the greatest hazards faced by mankind. Eruptive sequences from caldera-forming eruptions at Ossipee ring complex, New Hampshire, and Lake City caldera, Colorado, reveal that magmas underwent crystal fractionation to produce a zoned silicic magma chamber in each case before caldera formation. At Ossipee, magmatic inclusions with resorbed phenocrysts and positive Eu anomalies demonstrate that magma replenishment caused chamber rejuvenation and the initiation of caldera collapse. At Lake City, two ignimbrite units associated with episodes of caldera collapse have mafic-rich bases; this indicates that these collapse events were initiated by mafic magma replenishment. A numerical model is developed that describes how magma chamber rejuvenation causes a reduction in crystal content, a decrease in gas pressure, and hence caldera collapse. During caldera formation at Ossipee and Lake City, magmas from progressively deeper levels in the chambers were erupted and intruded to shallower levels. Periods of reverse compositional zonation and lateral compositional variation at the top of ignimbrite units and in post-collapse intrusions indicate that a period of accelerated magma interaction occurred in the chambers towards the end of subsidence. Scaled analogue experiments of caldera collapse into density-stratified magma chambers reveal a similar period of reverse zonation and dynamic fluid interaction as the subsiding block approaches the chamber base. Additionally, the experiments indicate that piecemeal or asymmetric collapse cause vortices to develop in the chamber which efficiently disrupt stratification. After caldera collapse at Ossipee and Lake City, replenishing magma caused mixed residual magma to intrude along caldera faults to shallow levels and drive resurgence. The work illustrates how particular magmatic processes influence caldera collapse, and in turn, how caldera collapse affects particular magmatic processes.
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Lichtblau, Andreas. "Stratigraphy and facies at the south margin of the Archean Noranda Caldera." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1989. http://theses.uqac.ca.

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Girard, Guillaume. "The dynamics of post-collapse magmatism at rhyolitic calderas: analogue experiments and geochemistry of Yellowstone lavas." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=40738.

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The dynamics of magma replenishment in silicic magma reservoirs are not well understood. This is an important issue, since replenishment may lead to the rapid accumulation of large volumes of crystal-poor magma, a condition potentially leading to cataclysmic caldera-forming eruptions. To shed light on this process, I have undertaken a combined experimental – geochemical approach designed to provide an integrated and synthetic view of magma replenishment processes. Scaled analogue experiments show that in silicic systems, buoyant injections rise through a magma reservoir without significant mixing with resident material, forming a layered reservoir. When a crystal mush is present at the base of the reservoir, its presence does not hinder buoyant injections to ascend. Indeed, such injections entrain crystals from the mush and transport them to the uppermost layers of the reservoir, resulting in the accumulation of a mix of replenishing magma and mush crystals. This process may have played a significant role in the generation of early post-collapse rhyolites of Yellowstone caldera, the Upper Basin Member rhyolites. In these lavas, I observe the coexistence of large, isolated, sieved plagioclase crystals with small, fresh, more calcic plagioclase crystals occurring as aggregates with pyroxenes and oxides. This unusual mineral assemblage suggests that a higher-temperature, more primitive silicic replenishing magma mixed with crystals from a mush shortly before eruption. In this scenario, the aggregates crystallized from the replenishing magma while the sieved crystals were extracted from the mush. Unlike the Upper Basin Member rhyolites, the younger voluminous Central Plateau Member rhyolites define a cogenetic series in which younger lavas exhibit more evolved mineralogy and trace element signatures, while crystal geochemistry suggests crystallization from progressively cooler melts. At the same time, the crystals also exhibit dissolution textures, suggesting a reh
La dynamique des recharges magmatiques dans les réservoirs de magma silicique est assez mal comprise. Ceci est un problème important, puisque les recharges magmatiques peuvent entraîner l’accumulation rapide de grands volumes de magma pauvre en cristaux, une configuration susceptible d’évoluer vers une éruption cataclysmique et la formation d’une caldeira. Pour comprendre ce processus, j’ai mené une approche combinant expériences et géochimie, afin d’obtenir une vision intégrée et synthétique du processus de recharges magmatiques. Des expériences analogiques dimensionnées montrent que, pour les systèmes siliciques, des injections de magma moins dense montent dans un réservoir magmatique sans se mélanger de façon significative avec le magma du réservoir, et forment un réservoir zoné. Lorsqu’un niveau saturé en cristaux est présent à la base du réservoir, sa présence n’empêche pas l’ascension des injections. En effet, ces injections moins denses arrachent des cristaux à ce niveau et les entraînent vers le toit du réservoir, où se forme une couche constituée d’un mélange du nouveau magma et de cristaux de la base du réservoir. Ce mécanisme a probablement joué un rôle clé dans la génèse des rhyolites post-caldeira précoces à Yellowstone, les rhyolites d’Upper Basin Member. Dans ces laves, j’observe une coexistence de grands cristaux de plagioclase isolés portant des textures en tamis, et de petits cristaux de plagioclase frais, plus calciques, présents en aggrégats avec des pyroxènes et des oxydes. Cette association inhabituelle suggère qu’un magma silicique plus primitif et plus chaud s’est mélangé à des cristaux d’un réservoir magmatique riche en cristaux peu avant son éruption. Dans ce modèle, les aggrégats ont cristallisé depuis le nouveau magma, et les cristaux à textures en tamis ont été arrachés au réservoir cristallin. Par opposition aux rhyolites d’Upper Basin Member, le
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Kerber, Paulo Augusto. "Granitic series and their economic geology." Thesis, Rhodes University, 1993. http://hdl.handle.net/10962/d1005581.

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The granitic rocks are subdivided into four series: tholeiitic, alkaline, calc-alkaline and mobilizates. These series can be formed from melting of mantle material (M-type granites) or from crustal rocks. There are granitic rocks formed from the mixing of these two magmas types. The rocks formed from crustal anatexis are subdivided into those formed from igneous rocks (I-type granites) and those formed from meta-sedimentary rocks (S-type granites). The former has similar characteristics to the mantle-derived granitoids. The mineral deposits related to igneous or mantle derived magma usually are Cu-Au, CUI Cu-Mo, Mo porphyries and have high oxygen fugacity and magnetic susceptibility (magnetite series). The Sn-W deposits usually are related to magma derived from meta-sedimentary or igneous rocks derived magma with low oxygen fugacity and magnetic susceptibility (ilmenite series). According to the tectonic setting, the granitoids rocks are classified as: Andino type, West Pacific type, Hercyno type, Caledonian type and Anorogenic (A-type granites).
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Grant, Mark. "Formation of Magmatic Fe-Ti-V-P Deposits Within the Lac St. Jean Area Saguenay, Québec, Canada: Insights from Trace Element Composition of Fe-Oxides and Apatite." Thesis, Université d'Ottawa / University of Ottawa, 2020. http://hdl.handle.net/10393/41253.

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The Lac St. Jean area in the Grenville Province of Quebec contains abundant anorthosite-hosted Fe-Ti-V and Fe-Ti-P mineralization comprised of massive to semi-massive Fe-oxides (magnetite ± ilmenite ± Al-spinel) and nelsonite (~2/3 oxide, ~1/3 apatite), respectively. Currently, information regarding regional-scale variation of mineralization, with respect to the composition of Fe-oxides, their relationship with host rocks, and genesis of the mineralization (i.e. immiscibility of a Fe-Ti ± P-rich magma vs. fractional crystallization) are not well constrained. In order to gain information into these enigmatic deposits, modern techniques involving in-situ laser ablation (LA)-ICP-MS analysis of Fe-oxides and apatite at the University of Ottawa combined with detailed petrography and whole rock lithogeochemistry were applied to samples from mineralization and host anorthosites from 2 Fe-Ti-V and 4 Fe-Ti-P deposits/occurrences. Results show that magnetite from Fe-Ti-P mineralization has a more evolved composition relative to magnetite from Fe-Ti-V mineralization. However, observed differences in; 1) relative abundance of Fe-oxide phases, 2) Fe-oxide exsolution textures, 3) visible corona-forming reactions with co-existing silicate phases (when present), and 4) whole rock compositions of corresponding massive oxide samples indicate possible post cumulus changes on primary composition of magnetite within each deposit/occurrence in this study. Post-cumulus processes appear to have a limited effect on the primary magmatic composition of apatite. Therefore, apatite appeared to be a robust indicator of primary magmatic compositions and was used to describe differences regarding the compositions of parental magma and oxygen fugacity (fO₂) conditions among the Fe-Ti-P deposits/occurrences. This study shows that, when combined with detailed petrography and whole rock lithogeochemistry, in-situ trace element composition of Fe-oxide minerals and apatite is a reliable indicator of the physiochemical conditions of the magmas which formed Fe-Ti-V and Fe-Ti-P mineralization within the Lac St. Jean area.
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Grill, Nicolette Deannah. "ECONOMIC GEOLOGY OF THE SAN BERNARDINO MOUNTAINS, CALIFORNIA." CSUSB ScholarWorks, 2014. https://scholarworks.lib.csusb.edu/etd/102.

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The San Bernardino Mountains are well known for their rich mining history, especially, gold in the mid-1800s and the current mining of one of the world’s largest deposits of high purity limestone. The purpose of this study was to compile new, current, and historical data of the major economic resources that are present and mining that has gone on in the San Bernardino Mountains. It is estimated that historical mining of the Holcomb Valley recovered $457,660,000 of gold or about 350,000 troy ounces based on samples collected for this study and 2013 gold price. The current major geologic resource is the limestone deposits on the north slope of the San Bernardino Mountains. Presently, there are three operators: Omya, Specialty Minerals, and Mitsubishi Cement. The San Bernardino Mountains are well known for skarn gold deposits. New work indicates that the placer gold from Holcomb Valley is often of very high purity. Placer gold samples were analyzed using the scanning electron microscope and energy dispersive x-ray spectra to determine the purity of the gold. Rim and core analysis of the placer gold was used to determine if the gold was transported from its source and to give an estimate of transportation distance. Results show some of the placer gold of Holcomb Valley has been rounded and flattened by weathering and transportation with increased gold purity in the rims while other gold grains still sustain their octahedral crystalline structure. Rims range in gold purity from 84.26% to 100%, with core gold purity ranging from 79.51% to 99.79%. Gold samples were weighed, photographed, measured, and classified by shape, angularity and texture, to assess the effects of transportation. Gold weights where used to calculate an economic value of gold. Geographic Information System “GIS” was used to visually display geology, historical and current mine locations, locations of samples used in this study, and to help calculate the volume of the Holcomb Valley TsE rock unit, which is where the placer gold is deposited. Sediment sample 15 from TsE had the lowest gold value of .002 ounces per cubic yard. This value is inferred to represent the amount of gold remaining after mining. Based on this assumption and the estimated volume of TsE at 50,027,000 cubic yards, the estimated total weight of gold remaining in the deposit is about 100,000 troy ounces, with a dollar value of about $130,760,000, using gold values for 2013. Sample 17 had the highest gold value, with .014 ounces per cubic yard. This is inferred to represent the concentration of placer gold deposits within parts of Holcomb Valley that have never been mined. This yields a total weight of the deposit of roughly 700,000 troy ounces, with an estimated value of $915,320,000 using gold prices for 2013. The gold values were calculated using November 7, 2013 gold spot price of $1,307.60.
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Willis-Richards, Jonathan. "Thermotectonics of the Cornubian batholith and their economic significance." Thesis, University of Exeter, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.259186.

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Mansolas, Ioannis. "Geochemistry and economic significance of the Pindos ophiolite mantle sequence." Thesis, Durham University, 1991. http://etheses.dur.ac.uk/6107/.

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In the Pindos ophiolite complex of northwestern Greece, mantle sequence peridotites comprise more than 90% of the exposed lithologies. At central Pindos, the complex is divided into two parts, northern and southern. Harzburgites, with little or no free clinopyroxene, are dominant in the latter, while clinopyroxene-bearing harzburgites are present in the former. The Moho is exposed in the southeast part of the southern block where cumulate rocks are in contact with mantle peridotite. The Moho has a transitional character and is characterized by increased abundance of discordant dunites, extensive emplacement of dykes of variable mineralogy, and the pervasive impregnation of the depleted harzburgite by basaltic melt. The cumulate rocks near this transition are dominated by dunite with subordinate troctolite and gabbro and minor wehrlite. There is no evidence of a well-developed magma chamber, with cumulates mostly appearing as sill-like bodies in a series of intrusions. Away from the Moho, cumulate olivine and two-pyroxene gabbros become abundant. Serpentinization has variably affected the peridotites but has not changed their major- element composition appreciably except for the addition of H(_2)O. A small depletion in the MgO wt.% content of the rocks is observed with increasing alteration, as well as mobilization of sulphur and re-distribution of sulphides. The complex has experienced two stages of re-equilibration at low pressures (<10 kb), the first between 850-950ºC, recorded by mineral equilibria with high-blocking temperatures, and the second at -750ºC, recorded by olivine-spinel pairs. The harzburgites show slightly elevated oxygen fugacities between QFM and QFM+1.5 (log units).The chemistry of the Pindos peridotites is quite variable. Comparison with peridotites from various geotectonic settings shows that the northern part of the complex has fairly uniform composition and experienced smaller degrees of partial melting in a mid-ocean ridge environment. The southern part is more depleted and resembles peridotites dredged from present-day intra-oceanic subduction zones. This is also supported by modelling of residues of partial melting of spinel Iherzolite using temperature- and pressure-dependent major- element distribution coefficients, showing degrees of melt extraction of the order of -12-15% and ~20%-40% for the northern and southern part respectively. The PGE content of the harzburgites is fairly uniform and similar to that of mantle- derived rocks world-wide. The abundance of the PGE is controlled by residual sulphides, while a small depletion in Pd is consistent with the presence of residual alloys. Chromitites have more variable PGE abundances and show both positive and gentle negative patterns. Oxygen fugacity and sulphide saturation are the controlling parameters of the abundances and patterns of the PGE.
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Shenk, Jonathan D., and Jonathan D. Shenk. "Economic geology of the White Cliffs diatomite deposit, Mammoth, Arizona." Thesis, The University of Arizona, 1990. http://hdl.handle.net/10150/558121.

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Books on the topic "Calderas Geology Geology, Economic"

1

Immitt, James Peter. Mineralización tipo skarn y vetas epitermales en la región de la Caldera de San Carlos, noreste de Chihuahua. Mexico, D.F: Ciudad Universitaria, 1987.

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Kokelaar, B. P. Classical areas of British geolopgy: Glencoe caldera volcano, Scotland. Nottingham: British Geological Survey, 2006.

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Mankinen, Edward A. Preliminary geomagnetic paleointensities from Long Valley Caldera, California. Menlo Park, CA: U.S. Geological Survey, 1994.

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Henry, Christopher D. The Van Horn Mountains caldera, Trans-Pecos, Texas: Geology and development of a small (10-km²) ash-flow caldera. Austin, Tex: Bureau of Economic Geology, Texas Mining and Mineral Resources Research Institute, University of Texas at Austin, 1986.

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Gluskoter, H. J., D. D. Rice, and R. B. Taylor, eds. Economic Geology, U.S. America: Geological Society of America, 1991. http://dx.doi.org/10.1130/dnag-gna-p2.

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Salas, Guillermo P., ed. Economic Geology, Mexico. Boulder, Colorado 80301: Geological Society of America, 1991. http://dx.doi.org/10.1130/dnag-gna-p3.

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J, Barron Eric, and Society of Economic Paleontologists and Mineralogists., eds. Paleoclimates and economic geology. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1986.

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Parrish, Judith Totman. Paleoclimates and economic geology. Tulsa, Okla: Societyof Economic Paleontologists and Mineralogists, 1986.

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Herath, J. W. Economic geology of Sri Lanka. 5th ed. Colombo: Ministry of Industrial Development, 1995.

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Herath, J. W. Economic geology of Sri Lanka. Colombo: Natural Resources, Energy & Science Authority, 1986.

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Book chapters on the topic "Calderas Geology Geology, Economic"

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Rock, N. M. S. "Economic Geology." In Lamprophyres, 150–56. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4757-0929-2_9.

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Rock, N. M. S. "Economic Geology." In Lamprophyres, 150–56. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4615-3924-7_9.

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Hart, Malcolm B. "Engineering & Economic Geology." In Applied Micropalaeontology, 225–62. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-017-0763-3_7.

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Varet, Jacques. "Geological Resources and Socio-Economic Issues." In Regional Geology Reviews, 295–321. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-60865-5_12.

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Dill, Harald G. "Pegmatitic Rocks and Economic Geology." In Modern Approaches in Solid Earth Sciences, 1–54. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-18806-5_1.

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Arndt, Nicholas, Stephen Kesler, and Clément Ganino. "The Future of Economic Geology." In Metals and Society, 173–99. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-17232-3_6.

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Arndt, Nicholas, and Clément Ganino. "The Future of Economic Geology." In Metals and Society, 141–51. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-22996-1_6.

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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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Wright, J. B. "Economic potential of the younger sedimentary basins." In Geology and Mineral Resources of West Africa, 114–20. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-015-3932-6_12.

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Mariano, A. N. "Chapter 11. ECONOMIC GEOLOGY OF RARE EARTH ELEMENTS." In Geochemistry and Mineralogy of Rare Earth Elements, edited by Bruce R. Lipin and G. A. McKay, 309–38. Berlin, Boston: De Gruyter, 1989. http://dx.doi.org/10.1515/9781501509032-014.

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Conference papers on the topic "Calderas Geology Geology, Economic"

1

Hovorka, Susan. "Global Status of Carbon Capture and Storage as a Greenhouse Gas Mitigation Measure." In Bureau of Economic Geology. US DOE, 2018. http://dx.doi.org/10.2172/1765821.

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Baybusinova, Z. B. "Risk Analysis & Economic Geology." In Saint Petersburg 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143759.

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Yang, Dayong, Zhiwei Xie, and Yingchun You. "Teaching Reform of Engineering Geology for Foreign Students." In 2017 International Conference on Education Science and Economic Management (ICESEM 2017). Paris, France: Atlantis Press, 2017. http://dx.doi.org/10.2991/icesem-17.2017.116.

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Young, Michael. "Update on Bureau of Economic Geology Research in Geological Sequestration." In TCEQ Trade Fair Austin, Texas May 2012. US DOE, 2012. http://dx.doi.org/10.2172/1747975.

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Hill, G. W. "The USGS Marine Geology Program in the Exclusive Economic Zone." In Offshore Technology Conference. Offshore Technology Conference, 1985. http://dx.doi.org/10.4043/4902-ms.

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Cehlar, Michal. "MODEL OF MINERAL DEPOSITS ECONOMIC EVALUATION." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.051.

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Weiss, Erik. "ECONOMIC EVALUATION OF USABILITY OF ABANDONED MINING WORKS." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s03.029.

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Cehlar, Michal. "ECONOMIC ANALYSIS OF POLYMETALLIC NODULES IN DEEP SEA FLOOR." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s03.028.

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Ruckova, Hana. "ECONOMIC EVALUTION OF POSSIBLE SCENARIOS FOR LARGE-SCALE EXCAVATOR REPLACEMENT." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.026.

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Cehlar, Michal. "TECHNOLOGICAL READINESS OF THE MINING PROJECT IN TERMS OF ECONOMIC PARAMETERS." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.081.

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Reports on the topic "Calderas Geology Geology, Economic"

1

mayr, U., T. de Freitas, and B. Beauchamp. Economic geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209776.

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Johnson, R. D., and N. J. McMillan. Petroleum [Chapter 6: Economic Geology]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192371.

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Cameron, A. R. Coal [Chapter 6: Economic Geology]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192372.

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Jessop, A. M. Geothermal energy [Chapter 6: Economic Geology]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192373.

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Aitken, J. D., and D. F. Stott. Metallic deposits [Chapter 6: Economic Geology]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192375.

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Sanford, B. V., A. W. Norris, and A. R. Cameron. Chapter 9: Hudson Platform - economic geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192379.

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Sanford, B. V. Chapter 12: St. Lawrence Platform - economic geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192382.

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Clague, J. J. Economic Implications of Quaternary Geology [Chapter 1: Quaternary Geology of the Canadian Cordillera]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127947.

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Musgrave, John A. Something Other Than a Career in Economic Geology. Office of Scientific and Technical Information (OSTI), May 2018. http://dx.doi.org/10.2172/1438099.

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Still, J. C., R. B. Hoekzema, T. K. Bundtzen, W. G. Gilbert, K. R. Wier, L. E. Burns, and S. A. Fechner. Economic geology of Haines-Klukwan-Porcupine area, southeastern Alaska. Alaska Division of Geological & Geophysical Surveys, 1991. http://dx.doi.org/10.14509/2478.

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