Data of Geochemistry Sixth Edition Chapter N
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Geochemistry - (2021-2022 Catalog) 1
Geochemistry - (2021-2022 Catalog) 1 GEGN586 NUMERICAL MODELING OF GEOCHEMICAL 3.0 Geochemistry SYSTEMS GEOL512 MINERALOGY AND CRYSTAL CHEMISTRY 3.0 Degrees Offered GEOL513 HYDROTHERMAL GEOCHEMISTRY 3.0 • Master of Science (Geochemistry) GEOL523 REFLECTED LIGHT AND ELECTRON 2.0 MICROSCOPY * • Doctor of Philosophy (Geochemistry) GEOL535 LITHO ORE FORMING PROCESSES 1.0 • Certificate in Analytical Geochemistry GEOL540 ISOTOPE GEOCHEMISTRY AND 3.0 • Professional Masters in Analytical Geochemistry (non-thesis) GEOCHRONOLOGY • Professional Masters in Environmental Geochemistry (non-thesis) GEGN530 CLAY CHARACTERIZATION 2.0 Program Description GEGX571 GEOCHEMICAL EXPLORATION 3.0 The Graduate Program in Geochemistry is an interdisciplinary program * Students can add one additional credit of independent study with the mission to educate students whose interests lie at the (GEOL599) for XRF methods which is taken concurrently with intersection of the geological and chemical sciences. The Geochemistry GEOL523. Program consists of two subprograms, administering two M.S. and Ph.D. degree tracks, two Professional Master's (non-thesis) degree programs, Master of Science (Geochemistry degree track) students must also and a Graduate Certificate. The Geochemistry (GC) degree track pertains complete an appropriate thesis, based upon original research they have to the history and evolution of the Earth and its features, including but not conducted. A thesis proposal and course of study must be approved by limited to the chemical evolution of the crust and -
The Central Kenya Peralkaline Province: Insights Into the Evolution of Peralkaline Salic Magmas
The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas. Ray Macdonald, Bruno Scaillet To cite this version: Ray Macdonald, Bruno Scaillet. The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas.. Lithos, Elsevier, 2006, 91, pp.1-4, 59-73. 10.1016/j.lithos.2006.03.009. hal-00077416 HAL Id: hal-00077416 https://hal-insu.archives-ouvertes.fr/hal-00077416 Submitted on 10 Jul 2006 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas R. Macdonalda, and B. Scailletb aEnvironment Centre, Lancaster University, Lancaster LA1 4YQ, UK bISTO-CNRS, 1a rue de la Férollerie, 45071 Orléans cedex 2, France Abstract The central Kenya peralkaline province comprises five young (< 1 Ma) volcanic complexes dominated by peralkaline trachytes and rhyolites. The geological and geochemical evolution of each complex is described and issues related to the development of peralkalinity in salic magmas are highlighted. The peralkaline trachytes may have formed by fractionation of basaltic magma via metaluminous trachyte and in turn generated pantellerite by the same mechanism. Comenditic rhyolites are thought to have formed by volatile-induced crustal anatexis and may themselves have been parental to pantelleritic melts by crystal fractionation. -
Organic Geochemistry
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ZENODO Organic Geochemistry Organic Geochemistry 37 (2006) 1–11 www.elsevier.com/locate/orggeochem Review Organic geochemistry – A retrospective of its first 70 years q Keith A. Kvenvolden * U.S. Geological Survey, 345 Middlefield Road, MS 999, Menlo Park, CA 94025, USA Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA Received 1 September 2005; accepted 1 September 2005 Available online 18 October 2005 Abstract Organic geochemistry had its origin in the early part of the 20th century when organic chemists and geologists realized that detailed information on the organic materials in sediments and rocks was scientifically interesting and of practical importance. The generally acknowledged ‘‘father’’ of organic geochemistry is Alfred E. Treibs (1899–1983), who discov- ered and described, in 1936, porphyrin pigments in shale, coal, and crude oil, and traced the source of these molecules to their biological precursors. Thus, the year 1936 marks the beginning of organic geochemistry. However, formal organiza- tion of organic geochemistry dates from 1959 when the Organic Geochemistry Division (OGD) of The Geochemical Soci- ety was founded in the United States, followed 22 years later (1981) by the establishment of the European Association of Organic Geochemists (EAOG). Organic geochemistry (1) has its own journal, Organic Geochemistry (beginning in 1979) which, since 1988, is the official journal of the EAOG, (2) convenes two major conferences [International Meeting on Organic Geochemistry (IMOG), since 1962, and Gordon Research Conferences on Organic Geochemistry (GRC), since 1968] in alternate years, and (3) is the subject matter of several textbooks. -
W. M. White Geochemistry Chapter 5: Kinetics
W. M. White Geochemistry Chapter 5: Kinetics CHAPTER 5: KINETICS: THE PACE OF THINGS 5.1 INTRODUCTION hermodynamics concerns itself with the distribution of components among the various phases and species of a system at equilibrium. Kinetics concerns itself with the path the system takes in T achieving equilibrium. Thermodynamics allows us to predict the equilibrium state of a system. Kinetics, on the other hand, tells us how and how fast equilibrium will be attained. Although thermo- dynamics is a macroscopic science, we found it often useful to consider the microscopic viewpoint in developing thermodynamics models. Because kinetics concerns itself with the path a system takes, what we will call reaction mechanisms, the microscopic perspective becomes essential, and we will very often make use of it. Our everyday experience tells one very important thing about reaction kinetics: they are generally slow at low temperature and become faster at higher temperature. For example, sugar dissolves much more rapidly in hot tea than it does in ice tea. Good instructions for making ice tea might then incor- porate this knowledge of kinetics and include the instruction to be sure to dissolve the sugar in the hot tea before pouring it over ice. Because of this temperature dependence of reaction rates, low tempera- ture geochemical systems are often not in equilibrium. A good example might be clastic sediments, which consist of a variety of phases. Some of these phases are in equilibrium with each other and with porewater, but most are not. Another example of this disequilibrium is the oceans. The surface waters of the oceans are everywhere oversaturated with respect to calcite, yet calcite precipitates from sea- water only through biological activity. -
The Role of Geochemistry and Stress on Fracture Development And
Geothermal Technologies Program 2010 Peer Review Public Service of Colorado Ponnequin Wind Farm The Role of Geochemistry and Principal Investigator (Joseph Moore) Stress on Fracture Development Presenter Name (John McLennan) and Proppant Behavior in EGS Organization University of Utah Reservoirs Track Name Reservoir Characterization May 18, 2010 This presentation does not contain any proprietary confidential,1 | US DOE or Geothermalotherwise restricted Program information. eere.energy.gov Timeline DOE Start Date:9/30/2008 DOE Contract Signed: 9/26/2008 Ends 11/30/2011 Project ~40% Complete 2 | US DOE Geothermal Program eere.energy.gov Budget Overview DOE Awardee Total Share Share Project $972,751 $243,188 $1,215,939 Funding FY 2009 $244,869 $107,130 $351,999 FY 2010 $383,952 $64,522 $448,474 FY 2011 $343,930 $71,536 $415,466 DOE Start Date:9/30/2008 DOE Contract Signed: 9/26/2008 Ends 11/30/2011 Project ~40% Complete 3 | US DOE Geothermal Program eere.energy.gov Overview: Barriers and Partners . Barriers to EGS Reservoir Development Addressed: . Reservoir Creation . Long-Term Reservoir and Fracture Sustainability . Zonal Isolation . Partners . Independent Evaluation 4 | US DOE Geothermal Program eere.energy.gov Relevance/Impact of Research Problem . Maximizing initial conductivity of EGS domains . Maintaining long-term conductivity . Facilitate development of extensive stimulated domain via diversion Solution . Proppant placed in fractures Challenge . Proppant behavior at geothermal conditions poorly understood Use of proppant recognized as potential technology under Task “Keep Flow Paths Open” in DOE EGS Technology Evaluation Report 5 | US DOE Geothermal Program eere.energy.gov Relevance/Impact of Research OBJECTIVE Develop Improved Methods For Maintaining Permeable Fracture Volumes In EGS Reservoirs . -
Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest
Chapter 21A. Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest Contribution by Robert D. Tucker, Harvey E. Belkin, Klaus J. Schulz, Stephen G. Peters, and Kim P. Buttleman Abstract The Khanneshin carbonatite is a deeply dissected igneous complex of Quaternary age that rises approximately 700 meters above the flat-lying Neogene sediments of the Registan Desert, Helmand Province, Afghanistan. The complex consists almost exclusively of carbonate-rich intrusive and extrusive igneous rocks, crudely circular in outline, with only three small hypabyssal plugs of leucite phonolite and leucitite outcropping in the southeastern part of the complex. The complex is broadly divisible into a central intrusive vent (or massif), approximately 4 kilometers in diameter, consisting of coarse-grained sövite and brecciated and agglomeratic barite-ankerite alvikite; a thin marginal zone (less than 1 kilometer wide) of outwardly dipping (5°–45°). Neogene sedimentary strata; and a peripheral apron of volcanic and volcaniclastic strata extending another 3–5 kilometers away from the central intrusive massif. Small satellitic intrusions of biotite-calcite carbonatite, no larger than 400 meters in diameter, crop out on the southern and southeastern margin of the central intrusive massif. In the 1970s several teams of Soviet geologists identified prospective areas of interest for uranium, phosphorus, and light rare earth element (LREE) mineralization in four regions of the carbonatite complex. High uranium concentrations are reported in two regions; the greatest concentrations are confined to silicified shear zones in sandy clay approximately 1.1 kilometers southwest of the peripheral part of the central vent. An area of phosphorus enrichment, primarily occurring in apatite, is present in coarse-grained agglomeratic alvikite, with abundant fenite xenoliths, approximately 750 meters south of the periphery of the central vent. -
Geology of the Nairobi Region, Kenya
% % % % % % % % %% %% %% %% %% %% %% % GEOLOGIC HISTORY % %% %% % % Legend %% %% %% %% %% %% %% % % % % % % HOLOCENE: %% % Pl-mv Pka %%% Sediments Mt Margaret U. Kerichwa Tuffs % % % % %% %% % Longonot (0.2 - 400 ka): trachyte stratovolcano and associated deposits. Materials exposed in this map % %% %% %% %% %% %% % section are comprised of the Longonot Ash Member (3.3 ka) and Lower Trachyte (5.6-3.3 ka). The % Pka' % % % % % % L. Kerichwa Tuff % % % % % % Alluvial fan Pleistocene: Calabrian % % % % % % % Geo% lo% gy of the Nairobi Region, Kenya % trachyte lavas were related to cone building, and the airfall tuffs were produced by summit crater formation % % % % % % % % % % % % % % % % % Pna % % % % %% % (Clarke et al. 1990). % % % % % % Pl-tb % % Narok Agglomerate % % % % % Kedong Lake Sediments Tepesi Basalt % % % % % % % % % % % % % % % % %% % % % 37.0 °E % % % % 36.5 °E % % % % For area to North see: Geology of the Kijabe Area, KGS Report 67 %% % % % Pnt %% % PLEISTOCENE: % % %% % % % Pl-kl %% % % Nairobi Trachyte % %% % -1.0 ° % % % % -1.0 ° Lacustrine Sediments % % % % % % % % Pleistocene: Gelasian % % % % % Kedong Valley Tuff (20-40 ka): trachytic ignimbrites and associated fall deposits created by caldera % 0 % 1800 % % ? % % % 0 0 % % % 0 % % % % % 0 % 0 8 % % % % % 4 % 4 Pkt % formation at Longonot. There are at least 5 ignimbrite units, each with a red-brown weathered top. In 1 % % % % 2 % 2 % % Kiambu Trachyte % Pl-lv % % % % % % % % % % %% % % Limuru Pantellerite % % % % some regions the pyroclastic glass and pumice has been -
Evolution of the Magma System of Pantelleria (Italy) from 190 Ka to Present
Eastern Kentucky University Encompass EKU Faculty and Staff Scholarship Faculty and Staff Scholarship Collection 2021 Evolution of the magma system of Pantelleria (Italy) from 190 ka to present. Nina J. Jordan University of Leicester John C. White Eastern Kentucky University, [email protected] Ray Macdonald University of Warsaw Silvio G. Rotolo Universita degli Studi di Palermo Follow this and additional works at: https://encompass.eku.edu/fs_research Part of the Geochemistry Commons, Geology Commons, and the Volcanology Commons Recommended Citation Nina J. Jordan; John C. White; Ray Macdonald; Silvio G. Rotolo. Evolution of the magma system of Pantelleria (Italy) from 190 ka to present. Comptes Rendus. Géoscience, Online first (2021), pp. 1-17. doi : 10.5802/crgeos.50. This Article is brought to you for free and open access by the Faculty and Staff Scholarship Collection at Encompass. It has been accepted for inclusion in EKU Faculty and Staff Scholarship by an authorized administrator of Encompass. For more information, please contact [email protected]. Comptes Rendus Géoscience Sciences de la Planète Nina J. Jordan, John C. White, Ray Macdonald and Silvio G. Rotolo Evolution of the magma system of Pantelleria (Italy) from 190 ka to present Online first (2021) <https://doi.org/10.5802/crgeos.50> Part of the Special Issue: Perspectives on alcaline magmas Guest editor: Bruno Scaillet (Institut des Sciences de la Terre d’Orléans, CNRS, France) © Académie des sciences, Paris and the authors, 2021. Some rights reserved. This article is licensed under the Creative Commons Attribution 4.0 International License. http://creativecommons.org/licenses/by/4.0/ Les Comptes Rendus. -
Tonnare in Italy: Science, History, and Culture of Sardinian Tuna Fishing 1
Tonnare in Italy: Science, History, and Culture of Sardinian Tuna Fishing 1 Katherine Emery The Mediterranean Sea and, in particular, the cristallina waters of Sardinia are confronting a paradox of marine preservation. On the one hand, Italian coastal resources are prized nationally and internationally for their natural beauty as well as economic and recreational uses. On the other hand, deep-seated Italian cultural values and traditions, such as the desire for high-quality fresh fish in local cuisines and the continuity of ancient fishing communities, as well as the demands of tourist and real-estate industries, are contributing to the destruction of marine ecosystems. The synthesis presented here offers a unique perspective combining historical, scientific, and cultural factors important to one Sardinian tonnara in the context of the larger global debate about Atlantic bluefin tuna conservation. This article is divided into four main sections, commencing with contextual background about the Mediterranean Sea and the culture, history, and economics of fish and fishing. Second, it explores as a case study Sardinian fishing culture and its tonnare , including their history, organization, customs, regulations, and traditional fishing method. Third, relevant science pertaining to these fisheries’ issues is reviewed. Lastly, the article considers the future of Italian tonnare and marine conservation options. Fish and fishing in the Mediterranean and Italy The word ‘Mediterranean’ stems from the Latin words medius [middle] and terra [land, earth]: middle of the earth. 2 Ancient Romans referred to it as “ Mare nostrum ” or “our sea”: “the territory of or under the control of the European Mediterranean countries, especially Italy.” 3 Today, the Mediterranean Sea is still an important mutually used resource integral to littoral and inland states’ cultures and trade. -
TCHAD : Carte De Référence Du Tibesti (Février 2018)
TCHAD : Carte de référence du Tibesti (février 2018) 13°0'0"E 14°0'0"E 15°0'0"E 16°0'0"E 17°0'0"E 18°0'0"E 19°0'0"E 20°0'0"E 21°0'0"E 22°0'0"E 23°0'0"E Curni Ebredaa Al Malaqi Gara Kourni Guelta Mouri Idie Mezafeh Eringi Kourini Ehi Ebesoua Askinoa Biligay 23°0'0"N Tourki Dao 23°0'0"N Bissan Ehi- Bardi Kidi Sigurian Fokiri Tehia Hamadat Mouri Idie Tega Askinoa Manghini Ehi Bissoa Eke Rhoan Fokioure Garako-Karamo Fokiri Tenere Gara Mezora Ehi Mozorki Ehi Fokiri Mali Dourdoura Bir el War Tanoa Odorloptina Domasaka Gara Dohonia ⛜ Oloseri Ehi Yohobe Tiri Ennedi Sanaka Yourokali Gege Kourini Kourina Ouadoi Ennri Sanaka Nangara Ehi Kourina Ziri Goubou Ehi Araye Ehi Aray Passe de Sidi Aidao Ehi Ehi Kourizo Korizo Agala Enneri Aray Dafora Ehi Agalla Tara Oske Enneri Ehi Loga Bai Darda-Morkena Talagoum Abou Ehi Tchouhi Enneri Ache Yebige Enneri Aozou Tuzugu Tioumi-Ahinoa Enneri Kakeron Lama-Kora Gara Lakor Ehi Tchoui Ehi Doma Dougouli Tebidi Tiohodoma Tirke Enneri Sogoyi L I B YE Lemakora Ehi Chilii Bordaa Ehi Chili Koundie Ehi Tihodoma Ennedi Gudu Ennedi Gadu Eoj Wahs Yourgor-Gara Afafi Plateau Col de Mechi Taba Enneri Taar Gebel Afafi Touside-Fosma Enneri Meche Dobious Looteni Koysono Ehi Sohayi Ehi Tekoukoue Enneri Ehi Madoa Ehi Nangara Soo Ehi Ehi Dogolaga Oudji-Emi Yedri Mine Morogue Koui Ergida Elliguemi Ehi Enneri Enneri Kasa Kourea Mamadou Enneri Arabi Sao Yedri Enneri Yedri Ehi Tchedona Ehi Domor Eligemi Dogologa Chedenemia Ehi Kourea-Momodoy Asaserde Oualasena Aray Yedri Tega Taar Fodogoroa Orda Afafi Galliema Enneri Enneri Enneri Fodogoroum -
Petroglyph National Monument: Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Petroglyph National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2017/1547 ON THE COVER Photograph of Albuquerque volcanoes. Three spatter cones, known as the Sisters, form a distinctive skyline west of Albuquerque, New Mexico. These small volcanoes are part of the Albuquerque volcanic field and occur in the Volcanoes area of Petroglyph National Monument. The volcanic field was active about 156,000 years ago. NPS photograph by Chanteil Walter (Petroglyph National Monument). THIS PAGE Photograph of the West Mesa escarpment along the Rinconada Canyon Trail. Erosion of the Santa Fe Group sediments that underlie a basaltic cap rock has caused large blocks of rock to tumble down the eastern escarpment of the mesa. Most of the petroglyphs were chiseled into the dark patina of desert varnish on these large boulders, exposing the lighter colored basaltic rock beneath. NPS photograph by Dale Pate (Geologic Resources Division). Petroglyph National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2017/1547 Katie KellerLynn Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 November 2017 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. -
Lunar Crater Volcanic Field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA)
Research Paper GEOSPHERE Lunar Crater volcanic field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA) 1 2,3 4 5 4 5 1 GEOSPHERE; v. 13, no. 2 Greg A. Valentine , Joaquín A. Cortés , Elisabeth Widom , Eugene I. Smith , Christine Rasoazanamparany , Racheal Johnsen , Jason P. Briner , Andrew G. Harp1, and Brent Turrin6 doi:10.1130/GES01428.1 1Department of Geology, 126 Cooke Hall, University at Buffalo, Buffalo, New York 14260, USA 2School of Geosciences, The Grant Institute, The Kings Buildings, James Hutton Road, University of Edinburgh, Edinburgh, EH 3FE, UK 3School of Civil Engineering and Geosciences, Newcastle University, Newcastle, NE1 7RU, UK 31 figures; 3 tables; 3 supplemental files 4Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, Ohio 45056, USA 5Department of Geoscience, 4505 S. Maryland Parkway, University of Nevada Las Vegas, Las Vegas, Nevada 89154, USA CORRESPONDENCE: gav4@ buffalo .edu 6Department of Earth and Planetary Sciences, 610 Taylor Road, Rutgers University, Piscataway, New Jersey 08854-8066, USA CITATION: Valentine, G.A., Cortés, J.A., Widom, ABSTRACT some of the erupted magmas. The LCVF exhibits clustering in the form of E., Smith, E.I., Rasoazanamparany, C., Johnsen, R., Briner, J.P., Harp, A.G., and Turrin, B., 2017, overlapping and colocated monogenetic volcanoes that were separated by Lunar Crater volcanic field (Reveille and Pancake The Lunar Crater volcanic field (LCVF) in central Nevada (USA) is domi variable amounts of time to as much as several hundred thousand years, but Ranges, Basin and Range Province, Nevada, USA): nated by monogenetic mafic volcanoes spanning the late Miocene to Pleisto without sustained crustal reservoirs between the episodes.