FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034971480> ?p ?o ?g. }

• W2034971480 endingPage "148" @default.
• W2034971480 startingPage "118" @default.
• W2034971480 abstract "The Tethyan Metallogenic Belt (TMB), extending from Europe through Anatolia to Iran, is one of the world's major metal producing belts, and consists of many sectors. Mineral deposits of the Biga Peninsula in northwestern Turkey exhibit, in many ways, the characteristics of mineral deposits found throughout the belt. Biga Peninsula tectonically forms the westernmost part of the Sakarya Zone and easternmost part of the Rhodope Zone at the intersection of Gondwana and Laurasia. The Biga Peninsula metallogeny research and exploration project created a GIS inventory of mineral deposits and prospects, and classified them genetically to evaluate the mineral deposit potential using genetic models based on descriptive data. The GIS database, consisting of 128 deposits or prospects, helped to generate new prospects and potential prospects. This field-based study indicated that the Biga Peninsula forms a prime target for gold–copper exploration not only in Turkey but in the world. The current economically significant mineral deposits of the Biga Peninsula were shaped by Cenozoic calc-alkaline magmatism, ranging between 52 and 18 Ma, and related to mainly collisional and post-collisional tectonic regime. Epithermal Au–Ag deposits including high-(HS), low-(LS) and intermediate-sulfidation (IS) styles, porphyry Au–Cu–Mo and base-metal skarn systems are economically the most important. Though there are no currently economic examples of some of them in the Biga Peninsula, other deposit types include Carlin-like distal disseminated Au–Ag, orogenic Au, especially listwanite hosted, volcanogenic Mn and U, lateritic (ferricrete) Fe deposits, carbonate replacement (CR) and placers. Several active metal mines, such as Balya, Arapucandere and Koru, are operating in the Biga Peninsula. Kucukdere Au–Ag deposit in Balikesir is the only gold mine in the Biga Peninsula, except for by-product gold produced from base-metal deposits. Results of the study show current total gold endowment of the Biga Peninsula including reserves and/or resources is 9.18 Moz gold [284.2 t] contained in twelve different deposits. Of these only 6 contain significant gold [> 0.3 Moz or 10 t]. Halilaga porphyry and Agi Dagi and Kirazli HS epithermal systems have an ongoing resource estimate, and Halilaga is a candidate to be one of the largest Cu–Au deposits not only in the Biga Peninsula, but in Turkey. Currently newly discovered Tepeoba is the largest porphyry Cu–Mo–Au deposit with known resources in the Biga Peninsula. Here, the first40Ar/39Ar step-heating age data conducted on some of the major HS epithermal gold deposits and causative intrusives in the Biga Peninsula are reported. Geochronological results from this project, evaluated with previous studies, indicate at least 3 phases of porphyry and 2 phases of high-sulfidation epithermal gold mineralization in the Biga Peninsula. The most important mineralizing phases and related host rocks for gold mineralization range from 38 to 22 Ma. The Oligocene is especially important for economic epithermal and porphyry systems in the Biga Peninsula, which is comparable to deposits in the Oligo-Miocene Serbomacedonian-Rhodope metallogenic belt of the Balkan Peninsula in SE Europe." @default.
• W2034971480 created "2016-06-24" @default.
• W2034971480 creator A5038494679 @default.
• W2034971480 date "2012-08-01" @default.
• W2034971480 modified "2023-10-01" @default.
• W2034971480 title "A prospective sector in the Tethyan Metallogenic Belt: Geology and geochronology of mineral deposits in the Biga Peninsula, NW Turkey" @default.
• W2034971480 cites W1616995146 @default.
• W2034971480 cites W1963540556 @default.
• W2034971480 cites W1969987147 @default.
• W2034971480 cites W1971331825 @default.
• W2034971480 cites W1983926551 @default.
• W2034971480 cites W1989767451 @default.
• W2034971480 cites W1990287569 @default.
• W2034971480 cites W1993235439 @default.
• W2034971480 cites W1998598291 @default.
• W2034971480 cites W1999754474 @default.
• W2034971480 cites W2003279842 @default.
• W2034971480 cites W2003419738 @default.
• W2034971480 cites W2009936725 @default.
• W2034971480 cites W2018123934 @default.
• W2034971480 cites W2018755912 @default.
• W2034971480 cites W2027287476 @default.
• W2034971480 cites W2028865941 @default.
• W2034971480 cites W2032912062 @default.
• W2034971480 cites W2044111361 @default.
• W2034971480 cites W2045594539 @default.
• W2034971480 cites W2048403692 @default.
• W2034971480 cites W2055949064 @default.
• W2034971480 cites W2057863618 @default.
• W2034971480 cites W2059466949 @default.
• W2034971480 cites W2062967308 @default.
• W2034971480 cites W2065204617 @default.
• W2034971480 cites W2067856311 @default.
• W2034971480 cites W2069495368 @default.
• W2034971480 cites W2075175050 @default.
• W2034971480 cites W2076104313 @default.
• W2034971480 cites W2077473835 @default.
• W2034971480 cites W2079902832 @default.
• W2034971480 cites W2081160716 @default.
• W2034971480 cites W2081466126 @default.
• W2034971480 cites W2081635584 @default.
• W2034971480 cites W2082700329 @default.
• W2034971480 cites W2085045756 @default.
• W2034971480 cites W2088440021 @default.
• W2034971480 cites W2089234747 @default.
• W2034971480 cites W2092068439 @default.
• W2034971480 cites W2095601024 @default.
• W2034971480 cites W2096707152 @default.
• W2034971480 cites W2106243060 @default.
• W2034971480 cites W2110613902 @default.
• W2034971480 cites W2115092464 @default.
• W2034971480 cites W2115550380 @default.
• W2034971480 cites W2119065610 @default.
• W2034971480 cites W2122562158 @default.
• W2034971480 cites W2131521566 @default.
• W2034971480 cites W2132065354 @default.
• W2034971480 cites W2142089274 @default.
• W2034971480 cites W2144222955 @default.
• W2034971480 cites W2148587619 @default.
• W2034971480 cites W2153210255 @default.
• W2034971480 cites W2157184090 @default.
• W2034971480 cites W2165394332 @default.
• W2034971480 cites W2168380098 @default.
• W2034971480 cites W2169262781 @default.
• W2034971480 cites W2170251510 @default.
• W2034971480 cites W2974031284 @default.
• W2034971480 doi "https://doi.org/10.1016/j.oregeorev.2011.09.015" @default.
• W2034971480 hasPublicationYear "2012" @default.
• W2034971480 type Work @default.
• W2034971480 sameAs 2034971480 @default.
• W2034971480 citedByCount "70" @default.
• W2034971480 countsByYear W20349714802012 @default.
• W2034971480 countsByYear W20349714802013 @default.
• W2034971480 countsByYear W20349714802014 @default.
• W2034971480 countsByYear W20349714802015 @default.
• W2034971480 countsByYear W20349714802016 @default.
• W2034971480 countsByYear W20349714802017 @default.
• W2034971480 countsByYear W20349714802018 @default.
• W2034971480 countsByYear W20349714802019 @default.
• W2034971480 countsByYear W20349714802020 @default.
• W2034971480 countsByYear W20349714802021 @default.
• W2034971480 countsByYear W20349714802022 @default.
• W2034971480 countsByYear W20349714802023 @default.
• W2034971480 crossrefType "journal-article" @default.
• W2034971480 hasAuthorship W2034971480A5038494679 @default.
• W2034971480 hasConcept C119127063 @default.
• W2034971480 hasConcept C123588078 @default.
• W2034971480 hasConcept C126457475 @default.
• W2034971480 hasConcept C127313418 @default.
• W2034971480 hasConcept C151730666 @default.
• W2034971480 hasConcept C156622251 @default.
• W2034971480 hasConcept C166957645 @default.
• W2034971480 hasConcept C17409809 @default.
• W2034971480 hasConcept C195843664 @default.
• W2034971480 hasConcept C202746551 @default.
• W2034971480 hasConcept C2776062231 @default.
• W2034971480 hasConcept C2776152364 @default.
• W2034971480 hasConcept C2776268066 @default.

• next