Academic literature on the topic 'Hydrothermal and continental sources'

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Journal articles on the topic "Hydrothermal and continental sources"

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Li, Weiqiang, Brian L. Beard, and Clark M. Johnson. "Biologically recycled continental iron is a major component in banded iron formations." Proceedings of the National Academy of Sciences 112, no. 27 (2015): 8193–98. http://dx.doi.org/10.1073/pnas.1505515112.

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Banded iron formations (BIFs) record a time of extensive Fe deposition in the Precambrian oceans, but the sources and pathways for metals in BIFs remain controversial. Here, we present Fe- and Nd-isotope data that indicate two sources of Fe for the large BIF units deposited 2.5 billion y ago. High-εNd and -δ56Fe signatures in some BIF samples record a hydrothermal component, but correlated decreases in εNd- and δ56Fe values reflect contributions from a continental component. The continental Fe source is best explained by Fe mobilization on the continental margin by microbial dissimilatory iron
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Yuan, Jingying, Haigang Cao, Yuping Guo, and Xuegang Chen. "Source and Evolution of Subduction–Related Hot Springs Discharged in Tengchong Geothermal Field, Southwest China: Constrained by Stable H, O, and Mg Isotopes." Minerals 12, no. 12 (2022): 1490. http://dx.doi.org/10.3390/min12121490.

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The hydrothermal system plays a crucial role in material and energy cycling between the lithosphere and hydrosphere. In general, seafloor hydrothermal systems are one of important Mg sinks, but the situation may not be the same as it is in terrestrial hydrothermal systems. In addition, the behavior of Mg isotopes during hydrothermal circulation is still unclear. Thus, in this study, we determined the Mg isotopic compositions of the hydrothermal fluids discharged in the Tengchong region to understand better the fate of Mg in the continental hydrothermal system. The δ2H and δ18O values of the Te
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Coltat, Rémi, Philippe Boulvais, Yannick Branquet, Antonin Richard, Alexandre Tarantola, and Gianreto Manatschal. "Moho carbonation at an ocean-continent transition." Geology 50, no. 3 (2021): 278–83. http://dx.doi.org/10.1130/g49363.1.

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Abstract Carbonation of mantle rocks during mantle exhumation is reported in present-day oceanic settings, both at mid-ocean ridges and ocean-continent transitions (OCTs). However, the hydrothermal conditions of carbonation (i.e., fluid sources, thermal regimes) during mantle exhumation remain poorly constrained. We focus on an exceptionally well-preserved fossil OCT where mantle rocks have been exhumed and carbonated along a detachment fault from underneath the continent to the seafloor along a tectonic Moho. Stable isotope (oxygen and carbon) analyses on calcite indicate that carbonation res
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Zinchuk, N. N. "CRUSTS OF WEATHERING AS BASIC SUPPLIERS OF TERRIGENOUS MATERIAL DURING FORMATION OF ANCIENT DIAMONDIFEROUS PLACERS." Proceedings of higher educational establishments. Geology and Exploration, no. 2 (April 30, 2018): 24–32. http://dx.doi.org/10.32454/0016-7762-2018-2-24-32.

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On the example of Mesozoic deposits of one of the main diamondiferous regions of the Siberian platform, basic suppliers of terrigenous material into the ancient diamondiferous placers under formation and their occurrences have been characterized. Special attention has been paid to characteristics of local sources of allothigenous material removal to sedimentation basins of the said period, the main of which were Middle-Late Triassic crusts of weathering on terrigenous-carbonate rocks, formations of trappean origin (dolerites, tuffs, tufogene thick layers) and kimberlites. Comparatively short t
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Chiaradia, Massimo, Lluís Fontboté, and Agustín Paladines. "Metal Sources in Mineral Deposits and Crustal Rocks of Ecuador (1° N–4° S): A Lead Isotope Synthesis." Economic Geology 99, no. 6 (2004): 1085–106. http://dx.doi.org/10.2113/econgeo.99.6.1085.

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Abstract Ecuador consists of terranes having both continental (Chaucha, Tahuin, Loja terranes) and oceanic (Macuchi, Alao, Salado terranes) affinity, which were accreted to the Amazon craton from Late Jurassic to Eocene. Four main magmatic arcs were formed by the subduction of the Farallon/Nazca plate since the Jurassic: a Jurassic continental arc on the western margin of the Amazon craton, a Jurassic island arc (Alao terrane), an early Tertiary island arc (Macuchi terrane), and a middle-late Tertiary continental arc encompassing the terranes of Macuchi, Chaucha, Tahuin, Loja, and Alao after c
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Ansari, Arif H., Veeru Kant Singh, Pankaj Kumar, et al. "Hydrogeochemistry, Geothermometry, and Sourcing of High Dissolved Boron, Tungsten, and Chlorine Concentrations in the Trans-Himalayan Hotsprings of Ladakh, India." Hydrology 10, no. 6 (2023): 118. http://dx.doi.org/10.3390/hydrology10060118.

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Boron (B) and Tungsten (W) are often found enriched in high-temperature geothermal waters associated with the development of subduction-related mafic to felsic arc magma. However, knowledge about the sourcing and transportation of these elements from such hydrothermal systems is sparse and ambiguous. Being the only active continental collision site in the world, the Trans-Himalaya offers a unique chance to study how continental collision sources the high boron and tungsten concentrations in geothermal fluids. This study investigated the distribution of trace elements, major cations, and anions
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Chugaev, A. V. "Orogenic Gold Deposits of Northern Transbaikalia, Russia: Geology, Age, Sources, and Genesis." Geochemistry International 62, no. 9 (2024): 909–78. http://dx.doi.org/10.1134/s0016702924700484.

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Abstract The paper presents newly obtained and summarizes preexisting data of long-term geochronological and isotope studies of orogenic mesothermal gold deposits in the world’s largest Lena metallogenic province and reviews interpretations of their genesis. Geochronologic data indicate that the gold mineralization was formed during three ore-forming Paleozoic events. The early Late Ordovician–Early Silurian (450–430 Ma) event produced the abundant veinlet—disseminated gold–sulfide mineralization in Neoproterozoic carbonaceous terrigenous–carbonate rocks of the Baikal–Patom foldbelt (BPB). The
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Wang, Zhigao, Wenyan Cai, Shunda Li, and Xuli Ma. "Magma Sources and Tectonic Settings of Concealed Intrusive Rocks in the Jinchang Ore District, Yanbian–Dongning Region, Northeast China: Zircon U–Pb Geochronological, Geochemical, and Hf Isotopic Evidence." Minerals 12, no. 6 (2022): 708. http://dx.doi.org/10.3390/min12060708.

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The Jinchang deposit is a large Au deposit in the Yanbian–Dongning region, in Northeast China, and is the product of magmatic–hydrothermal activities related to Early Cretaceous concealed igneous intrusions. However, these Early Cretaceous ore-causative igneous intrusions and the ore-hosting rocks in the Jinchang ore district have rarely been studied, with their magma sources and tectonic settings being ambiguous. Here, we integrate new geochemical, zircon U–Pb and Hf isotopic data from the concealed ore-hosting monzogranite and the ore-causative granodiorite to constrain their magma sources a
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Ma, Guoxiong, Xiaobo Zhao, Chunji Xue, and Renke Wang. "Neoproterozoic Aksu Diabase Dyke, Chinese South Tianshan: Magma Sources and Implications for Regional Gold Metallogeny." Minerals 13, no. 3 (2023): 326. http://dx.doi.org/10.3390/min13030326.

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Tianshan is one of the world’s largest gold provinces; however, the relationship between gold mineralization and metasomatized subcontinental lithospheric mantle (SCLM) remains poorly understood. To improve our understanding, we present new bulk-rock geochemistry and platinum group element (PGE) concentrations of the SCLM-sourced Aksu Neoproterozoic diabase dykes in Chinese South Tianshan. These data, combined with in situ laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analyses of hydrothermal pyrite grains in the diabase dykes, are used to discuss the SCLM source char
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Peverelli, Veronica, Alfons Berger, Martin Wille, et al. "Multifaceted orogenic fluid dynamics unraveled by hydrothermal epidote." European Journal of Mineralogy 36, no. 5 (2024): 879–98. http://dx.doi.org/10.5194/ejm-36-879-2024.

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Abstract. Characterizing fluid circulation in orogens is key to understanding orogenic processes because fluid–rock interaction modifies the physical properties of rocks, hence their response to deformation and, for example, their suitability for radioactive waste storage. Fluid circulation can be dated by applying geochronological methods to fluid-precipitated minerals. Fluid sources and associated pathways can be traced using isotope data measured in the same or in other cogenetic minerals. We applied this concept to the Aar Massif (central Swiss Alps), which was part of the former European
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Dissertations / Theses on the topic "Hydrothermal and continental sources"

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Aquila, Quentin. "Explorer la géochimie des océans archéens avec les Formations de fer rubanées (BIF) : apport des compositions isotopiques Hf-Nd-Pb." Electronic Thesis or Diss., Université Clermont Auvergne (2021-...), 2024. http://www.theses.fr/2024UCFA0054.

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Les Formations de fer Rubanées (BIF) sont des archives sédimentaires uniques pour étudier les océans primitifs de l'Archéen. Cependant, l'environnement de formation et les mécanismes en jeu dans la formation de ces sédiments chimiques riches en fer et en silicium sont peu contraints. Les BIF ont été très peu étudiés pour leurs compositions isotopiques en Nd-Hf alors qu'elles pourraient permettre d'apporter de nouvelles contraintes sur les sources hydrothermales et continentales alimentant les anciens océans. Pour mieux contraindre l'environnement de formation des BIF, j'ai combiné des aspects
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Lopez, Benjamin. "Architecture et distribution des systemes carbonatés se développant autour des sources hydrothermales : cas d’étude du basin de Denizli (Turquie), de la region de Rapolano (Italie) et de Mammoth Hot Springs (Wyoming, USA)." Thesis, Aix-Marseille, 2015. http://www.theses.fr/2015AIXM4326.

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Les carbonates de sources hydrothermales (ou Geothermal Spring Carbonate, GSC) sont des systèmes carbonatés qui se développent autour de sources dont les eaux ont circulé en profondeur et sont remontées le long de failles perméables. Leur développement est contrôlé en tout premier lieu par la nature des eaux souterraines auxquelles ils sont liés. La formation de ces carbonates dépend d’interactions complexes entre les processus hydrologiques, tectoniques et structuraux se produisant avant l’émergence. Par la suite, la sédimentation est régie par de nombreux processus résultant des variations h
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Mercer, Celestine Nicole. "Mineralogical indicators of magmatic and hydrothermal processes in continental arc crust /." Connect to title online (Scholars' Bank) Connect to title online (ProQuest), 2009. http://hdl.handle.net/1794/10250.

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Mercer, Celestine Nicole 1979. "Mineralogical indicators of magmatic and hydrothermal processes in continental arc crust." Thesis, University of Oregon, 2009. http://hdl.handle.net/1794/10250.

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xviii, 177 p. : ill., maps. A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.<br>This dissertation explores several important consequences of H 2 O-rich fluids in magmatic and ore-forming systems within continental arc crust. North Sister, a stratovolcano in the Oregon High Cascades, provides a window into magma generation processes in the deep crust. Eruption of a remarkably limited basaltic andesite composition over the lifespan of this volcano may reflect last equilibration of mantle derived magma within a de
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Le, Gal Virginie. "Traçage thermique et géochimique des systèmes hydrothermaux : exemple d'un domaine océanique jeune et d'une marge continentale." Electronic Thesis or Diss., Paris 6, 2017. https://theses.hal.science/tel-01886790.

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Résumé Les processus hydrothermaux affectent l'ensemble des domaines océaniques et contrôlent efficacement leur régime thermique. Cependant, les études de flux de chaleur à l'échelle globale conduisent à des interprétations parfois en contradiction avec les études locales. Il est donc essentiel de comparer les effets de l'hydrothermalisme dans différents contextes régionaux. Dans cette optique, nous avons étudié le rôle de l'hydrothermalisme sur le régime thermique d'un domaine océanique jeune (en Atlantique) et d'une marge continentale jeune (Sud Baléares). Pour cela, nous avons quantifié les
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Cook, James Matthew. "Mid-fifteenth-century English mass cycles in continental sources." Thesis, University of Nottingham, 2014. http://eprints.nottingham.ac.uk/30778/.

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Fifteenth-century English music had a profound impact on mainland Europe, with several important innovations (e.g. the cyclic cantus firmus Mass) credited as English in origin. However, the turbulent history of the Church in England has left few English sources for this deeply influential repertory. The developing narrative surrounding apparently English technical innovations has therefore often focussed on the recognition of English works in continental manuscripts, with these efforts most recently crystallised in Curtis and Wathey's 'Fifteenth-Century English Liturgical Music: A List of the
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Le, Gal Virginie. "Traçage thermique et géochimique des systèmes hydrothermaux : exemple d'un domaine océanique jeune et d'une marge continentale." Thesis, Paris 6, 2017. http://www.theses.fr/2017PA066530/document.

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Résumé Les processus hydrothermaux affectent l'ensemble des domaines océaniques et contrôlent efficacement leur régime thermique. Cependant, les études de flux de chaleur à l'échelle globale conduisent à des interprétations parfois en contradiction avec les études locales. Il est donc essentiel de comparer les effets de l'hydrothermalisme dans différents contextes régionaux. Dans cette optique, nous avons étudié le rôle de l'hydrothermalisme sur le régime thermique d'un domaine océanique jeune (en Atlantique) et d'une marge continentale jeune (Sud Baléares). Pour cela, nous avons quantifié les
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Tizzard, Louise Helen. "The Contribution to atmospheric methane from sub-seabed sources in the UK continental shelf." Thesis, University of Newcastle upon Tyne, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.445613.

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Qu, Zihan. "Chemical properties of continental aerosol transported over the Southern Ocean : Patagonian and Namibian sources." Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066002/document.

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Patagonie et la Namibie sont deux sources importantes d'aérosol minéral qui alimente la section Atlantique Sud de l'océan Austral avec les micronutriments.L'objet de ma thèse est d'étudier 1) la concentration atmosphérique et la variation temporel de la poussière en Patagonie, 2) l'hétérogénéité spatiale de composition élémentaire de poussière en Patagonie et en Namibie, et 3) la solubilité élémentaire de poussière en Patagonie et en Namibie. Ces trois aspects sont les principaux enjeux pour modéliser les inventaires des émissions de micronutriments biodisponibles à partir de sources de poussi
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Qu, Zihan. "Chemical properties of continental aerosol transported over the Southern Ocean : Patagonian and Namibian sources." Electronic Thesis or Diss., Paris 6, 2016. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2016PA066002.pdf.

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Patagonie et la Namibie sont deux sources importantes d'aérosol minéral qui alimente la section Atlantique Sud de l'océan Austral avec les micronutriments.L'objet de ma thèse est d'étudier 1) la concentration atmosphérique et la variation temporel de la poussière en Patagonie, 2) l'hétérogénéité spatiale de composition élémentaire de poussière en Patagonie et en Namibie, et 3) la solubilité élémentaire de poussière en Patagonie et en Namibie. Ces trois aspects sont les principaux enjeux pour modéliser les inventaires des émissions de micronutriments biodisponibles à partir de sources de poussi
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Books on the topic "Hydrothermal and continental sources"

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Lucien, Laubier, Centre national de la recherche scientifique (France), Institut français de recherche pour l'exploitation de la mer., and Colloque "les sources hydrothermales de la ride du Pacifique oriental, biologie et écologie" (1985 : Institut océanographique, Paris), eds. Biologie et écologie des sources hydrothermales =: Biology and ecology of the hydrothermal vents : Institut océanographique - Paris, 4-7 novembre 1985. Gauthier-Villars, 1988.

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Saco, Alfredo. Difusión continental del aprismo. Okura Editores, 1985.

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Andrew, Wachtel, ed. Petrushka: Sources and contexts. Northwestern University Press, 1998.

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Umberto, Leanza, Sico Luigi, Ciciriello Maria Clelia, II Università degli studi di Roma., and Università di Napoli, eds. Mediterranean continental shelf: Delimitations and regimes : international and legal sources. Oceana Publications, 1988.

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Christie's. Genre: Victorian and 19th century continental pictures from various sources. Christie's, 1998.

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World Clean Energy Conference (1991 Geneva, Switzerland). Cleaner energy for sustainable development: Proceedings of the World Clean Energy Conference, World Energy Coalition for the global energy charter : Geneva International Conference Centre, 4-7 November 1991. Cercle mondial du consensus = World Circle of the Consensus, 1991.

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International, Workshop on Water Dynamics (5th 2007 Sendai-shi Miyagi-ken Japan). Water dynamics: 5th International Workshop on Water Dynamics, Sendai, Japan, 25-27 September 2007. American Institute of Physics, 2008.

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Platonov, Andreĭ Platonovich. The foundation pit. Northwestern University Press, 1994.

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United States. Congress. House. Committee on Natural Resources. Subcommittee on Energy and Mineral Resources., ed. Renewable energy opportunities and issues on the outer continental shelf: Joint oversight hearing before the Subcommittee on Fisheries, Wildlife, and Oceans, joint with the Subcommittee on Energy and Mineral Resources of the Committee on Natural Resources, U.S. House of Representatives, One Hundred Tenth Congress, first session, Tuesday, April 24, 2007. U.S. G.P.O., 2007.

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Platonov, Andreĭ Platonovich. Kotlovan: Tekst, materialy tvorcheskoĭ istorii. Nauka, 2000.

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Book chapters on the topic "Hydrothermal and continental sources"

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Pirajno, Franco. "Hydrothermal Mineral Deposits of Continental Rift Environments." In Hydrothermal Mineral Deposits. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-75671-9_14.

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Nieva, David, Rosa María Barragán, and Víctor Arellano. "Geochemistry of Hydrothermal Systems." In Power Stations Using Locally Available Energy Sources. Springer New York, 2018. http://dx.doi.org/10.1007/978-1-4939-7510-5_306.

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Sim, Stuart. "A Brief Pre-history of Super-Scepticism: Sources and Influences." In Contemporary Continental Philosophy. Routledge, 2021. http://dx.doi.org/10.4324/9781315200293-3.

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Eidel, J. J., and C. Meyer. "Scientific Drilling to Study the Roots and Margins of Hydrothermal Mineral Systems." In Exploration of the Deep Continental Crust. Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-45601-5_10.

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Nielson, Dennis L., and Jeffrey B. Hulen. "Observations in an Active Hydrothermal System Through Deep Drilling: Valles Caldera, New Mexico." In Exploration of the Deep Continental Crust. Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-45601-5_21.

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Schreiber, Ulrich C., and Christian Mayer. "The New Model: Hydrothermal Systems in the Early Continental Crust." In The First Cell. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-45381-7_7.

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Schreiber, Ulrich C., and Christian Mayer. "A Hypothetical Approach: Hydrothermal Systems in the Early Continental Crust." In The First Cell. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-45381-7_8.

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Fournier, Robert O. "Continental Scientific Drilling to Investigate Brine Evolution and Fluid Circulation in Active Hydrothermal Systems." In Exploration of the Deep Continental Crust. Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-45601-5_9.

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Huo, Zhibao. "Highly Selective Hydrothermal Production of Cyclohexanol from Biomass-Derived Cyclohexanone Over Cu Powder." In Diverse Hydrogen Sources for Biomass-derivatives Conversion. Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-1673-3_8.

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Storey, Michael, John J. Mahoney, and Andrew D. Saunders. "Cretaceous Basalts in Madagascar and the Transition Between Plume and Continental Lithosphere Mantle Sources." In Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm100p0095.

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Conference papers on the topic "Hydrothermal and continental sources"

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Kelechi, F. M., and O. I. Owoka. "The Future Perspective: Geothermal Energy in Nigeria – An Option to be Explored." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/217204-ms.

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Abstract As the transition towards a green energy future intensifies, cleaner energy sources are expected to drive the decline in the demand for fossil fuels. This creates room for renewable energy sources such as geothermal. Geothermal energy is generated from the earth's crust which is transported through cracks and fractures in the host rocks and its natural fluids at temperatures above the ambient level. The rate of heat flow in the crust is estimated to be 59Mw/m2 [1.9*10-2 Btu/h/ft2]. In mature continental cratons, the geothermal gradient can be as low as 10 °C per kilometer. However, in
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Scholz, Christopher A. "Advancing Models of Facies Variability and Lacustrine Source Rock Accumulation in Rifts: Implications for Exploration." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2577056-ms.

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ABSTRACT Important syn-rift hydrocarbon discoveries in the Tertiary East African Rift and in the South Atlantic subsalt basins have in recent years promoted renewed interest in the variability of source and reservoir rock facies in continental rifts. This talk considers several important new observations and developments in our understanding of the sedimentary evolution of lacustrine rift basins. Offshore subsalt basins in the South Atlantic demonstrate the importance of lacustrine carbonates, and especially microbialites, as reservoir facies in extensional systems. The role of rift-related ma
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Andrade-Barahona, Eva, and Alysia Cox. "Copper and iron uptake in continental hydrothermal systems." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.13652.

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Zakharov, David, Dmitry Zozulya, Daniela Rubatto, Dylan Colon, and Johanna Marin-Carbonne. "NEOARCHEAN CONTINENTAL EXPOSURE AND HYDROLOGICAL CYCLE RECORDED IN A 2.67 GA MAGMATIC-HYDROTHERMAL SYSTEM." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-365415.

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Rzonca, Bartlomiej, and Dirk Schulze-Makuch. "Investigation of hydrothermal sources in the Rio Grande rift region." In 53rd Annual Fall Field Conference. New Mexico Geological Society, 2002. http://dx.doi.org/10.56577/ffc-53.319.

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Follmann, Jörg, Froukje van der Zwan, Sven Petersen, and Matthias Frische. "Hydrothermal mineralization at continental breakup - geochemical insights from sulfide minerals from the South China Sea." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11378.

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Silaev, Valeriy Ivanovich, Irina Grigorievna Dobretsova, Anna Ivanovna Antoshkina, et al. "Hydrothermal sulfide mines in the Russian exploration area of the Middle Atlantic Ridge." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. ПЕРМСКИЙ ГОСУДАРСТВЕННЫЙ НАЦИОНАЛЬНЫЙ ИССЛЕДОВАТЕЛЬСКИЙ УНИВЕРСИТЕТ, 2022. http://dx.doi.org/10.17072/chirvinsky.2022.226.

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The results of new studies of sulfide mineralization from the rift valley of the Mid-Atlantic Ridge are considered. The regularities of the chemical and mineral composition, the peculiarities of mineralogical zoning at the local and regional scales are analyzed. The genetic aspects of the isotopic composition of sulfur and carbon in the products of oceanic and continental volcanism are discussed.
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Mingyuan Zhu, Yibo Yang, Yemin Hu, Ying Li, and Hongming Jin. "Preparation of MnO2 nanoflakes on Ti substrate by hydrothermal method." In 8th International Vacuum Electron Sources Conference and Nanocarbon (2010 IVESC). IEEE, 2010. http://dx.doi.org/10.1109/ivesc.2010.5644157.

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Yun-Chieh Yeh, Di-Yan Wang, and Chun-Wei Chen. "Work function evolution of graphene oxide by utilizing hydrothermal treatment." In 8th International Vacuum Electron Sources Conference and Nanocarbon (2010 IVESC). IEEE, 2010. http://dx.doi.org/10.1109/ivesc.2010.5644196.

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Cao, Wenrong, and Cin-Ty A. Lee. "SCALING ANALYSIS AND NUMERICAL MODELING OF HYDROTHERMAL CIRCULATION IN COOLING AND EXHUMING HOT CONTINENTAL ARC CRUST." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302219.

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Reports on the topic "Hydrothermal and continental sources"

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Davis, K. J., S. J. Richardson, and N. L. Miles. A virtual tall tower network for understanding continental sources and sinks of CO2. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/900564.

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Leet, R. C. Investigation of hydrothermal boiling and steam quenching as possible sources of volcanic tremor and geothermal ground noise. Office of Scientific and Technical Information (OSTI), 1991. http://dx.doi.org/10.2172/5524334.

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Goff, F. Caldera processes and magma-hydrothermal systems continental scientific drilling program: thermal regimes, Valles caldera research, scientific and management plan. Edited by D. L. Nielson. Office of Scientific and Technical Information (OSTI), 1986. http://dx.doi.org/10.2172/5467724.

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Petty, S., B. J. Livesay, W. P. Long, and J. Geyer. Supply of geothermal power from hydrothermal sources: A study of the cost of power in 20 and 40 years. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/6961102.

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Hulen, J. B., and D. L. Nielson. Hydrothermal brecciation in the Jemez Fault zone, Valles Caldera, New Mexico: Results from CSDP (Continental Scientific Drilling Program) corehole VC-1. Office of Scientific and Technical Information (OSTI), 1987. http://dx.doi.org/10.2172/6386155.

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Paradis, S., G. J. Simandl, N. Drage, R J D'Souza, D. J. Kontak, and Z. Waller. Carbonate-hosted deposits (Mississippi Valley-type, magnesite, and REE-F-Ba) of the southeastern Canadian Cordillera: a review and isotopic data comparison. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327995.

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The Mississippi Valley-type, magnesite, and REE-F-Ba deposits in the southeastern Canadian Cordillera are in the weakly deformed/metamorphosed Paleozoic carbonate platform of the Rocky Mountains. Most are hosted in dolostones of the middle Cambrian Cathedral, upper Cambrian Jubilee, and Upper Devonian Palliser formations and spatially associated with hydrothermal dolomite. They occur along structurally controlled facies transitions between the shallow-water carbonate platform and deeper water basin rocks of the Paleozoic continental margin. Their location and morphology reflect episodic riftin
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Vaughan, W. C., Frederick A. Bowles, and Joshua W. Chatelain. Compilation of Data Sources Used to Construct Bottom-Sediment Province Maps for the United States East Coast Continental Shelf from Cape Kennedy to Cape Hatteras and for Various Indonesian Waters. Defense Technical Information Center, 2004. http://dx.doi.org/10.21236/ada429967.

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Scanlan, E. J., M. Leybourne, D. Layton-Matthews, A. Voinot, and N. van Wagoner. Alkaline magmatism in the Selwyn Basin, Yukon: relationship to SEDEX mineralization. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328994.

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Several sedimentary exhalative (SEDEX) deposits have alkaline magmatism that is temporally and spatially associated to mineralization. This report outlines interim data from a study of potential linkages between magmatism and SEDEX mineralization in the Selwyn Basin, Yukon. This region is an ideal study site due to the close spatial and temporal relationships between SEDEX deposits and magmatism, particularly in the MacMillan Pass, where volcanic rocks have been drilled with mineralization at the Boundary deposit. Alkaline volcanic samples were analysed from the Anvil District, MacMillan Pass,
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Jefferson, C. W., S. Pehrsson, V. Tschirhart, et al. Geology and metallogeny of the northeast Thelon Basin region, Nunavut, and comparison with the Athabasca Basin, Saskatchewan. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332499.

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Based on extensive remapping of the northeast Thelon Basin region in Nunavut, uranium exploration criteria are adapted from those of the Athabasca Basin in Saskatchewan, as basin-specific paradigms. The Athabasca Basin straddles the Rae and Hearne cratons and the Taltson magmatic zone, whereas the Thelon Basin rests entirely within the Rae Craton. In the Athabasca Basin, four unconformity-bounded siliciclastic sequences with different paleocurrents record a complex depositional history, whereas the Thelon Formation is a single, albeit cyclic siliciclastic unit with uni-modal paleocurrents. Ben
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Kindt, Roeland, Ian K Dawson, Jens-Peter B Lillesø, Alice Muchugi, Fabio Pedercini, and James M Roshetko. The one hundred tree species prioritized for planting in the tropics and subtropics as indicated by database mining. World Agroforestry, 2021. http://dx.doi.org/10.5716/wp21001.pdf.

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A systematic approach to tree planting and management globally is hindered by the limited synthesis of information sources on tree uses and species priorities. To help address this, the authors ‘mined’ information from 23 online global and regional databases to assemble a list of the most frequent tree species deemed useful for planting according to database mentions, with a focus on tropical regions. Using a simple vote count approach for ranking species, we obtained a shortlist of 100 trees mentioned in at least 10 of our data sources (the ‘top-100’ species). A longer list of 830 trees that
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