FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2912137208> ?p ?o ?g. }

• W2912137208 endingPage "425" @default.
• W2912137208 startingPage "337" @default.
• W2912137208 abstract "Turkey, located within the western Tethyan-Eurasian Belt contains numerous porphyry copper deposits formed by the subduction, collision and post-collisional events during the closure of NeoTethys Ocean between the latest Cretaceous and late Miocene. These porphyry systems and associated epithermal and skarn deposits are associated with the subduction and post-subduction magmatic rocks emplaced along arc-parallel belts as in eastern Pontides and arc transverse extensional terranes as in the western Anatolian province (WAP) and Southeastern Anatolian Orogenic Belt (SEAOB). The porphyry deposits are formed in magmatic-arc (Pontides, Aegean and Bitlis-Zagros subduction), post-collisional settings (Pontides, WAP, SEAOB) after continental collision (Central Anatolian Crystalline Complex), and extensional arc setting (WAP). The porphyry Cu systems begin in the Late Cretaceous at the north, and generally young southward, where paired Late Cretaceous and Eocene metallogenic episodes are present in the eastern Pontides, WAP and SEAOB. The dominance of ages between ca. 83 and 70 Ma broadly coincides with the final stages of Late Cretaceous magmatism at the Pontides and SEAOB. The available ages are indicative of epidocity and a limited period of formation for porphyry Cu systems in these belts, and comparable to the metallogenic evolution of Turkey. The Eocene porphyry systems in discontinuous belts across Turkey reflect collisional to post-collisional processes. The number of known porphyry deposits in porphyry belts is related to the level of erosion. Therefore, the magmatic belts with fewer known porphyry may indicate too shallow or too deep crustal levels for their exposure. The estimates of numbers of undiscovered deposits combined with grade and tonnage models in Monte Carlo simulation revealed a lower density of known porphyry deposits in the Pontides, WAP and SEAOB relative to well-explored provinces around the world. This suggests that undiscovered deposits are likely present in Pontides, WAP and SEAOB." @default.
• W2912137208 created "2019-02-21" @default.
• W2912137208 creator A5027114387 @default.
• W2912137208 creator A5033375401 @default.
• W2912137208 creator A5044548903 @default.
• W2912137208 date "2019-01-01" @default.
• W2912137208 modified "2023-09-26" @default.
• W2912137208 title "Porphyry-Cu Deposits of Turkey" @default.
• W2912137208 cites W1537918871 @default.
• W2912137208 cites W1850526270 @default.
• W2912137208 cites W1879089888 @default.
• W2912137208 cites W1942202237 @default.
• W2912137208 cites W1963515656 @default.
• W2912137208 cites W1964993841 @default.
• W2912137208 cites W1965877299 @default.
• W2912137208 cites W1968318197 @default.
• W2912137208 cites W1970766209 @default.
• W2912137208 cites W1971002974 @default.
• W2912137208 cites W1971553849 @default.
• W2912137208 cites W1972663134 @default.
• W2912137208 cites W1974490503 @default.
• W2912137208 cites W1974501258 @default.
• W2912137208 cites W1974553500 @default.
• W2912137208 cites W1975719353 @default.
• W2912137208 cites W1976166881 @default.
• W2912137208 cites W1978049764 @default.
• W2912137208 cites W1979683866 @default.
• W2912137208 cites W1979705656 @default.
• W2912137208 cites W1980095243 @default.
• W2912137208 cites W1982067367 @default.
• W2912137208 cites W1983637112 @default.
• W2912137208 cites W1987883074 @default.
• W2912137208 cites W1988322715 @default.
• W2912137208 cites W1991249933 @default.
• W2912137208 cites W1992924010 @default.
• W2912137208 cites W1995011208 @default.
• W2912137208 cites W1995555849 @default.
• W2912137208 cites W1997468419 @default.
• W2912137208 cites W1997952954 @default.
• W2912137208 cites W2001387840 @default.
• W2912137208 cites W2001947407 @default.
• W2912137208 cites W2002166036 @default.
• W2912137208 cites W2002501800 @default.
• W2912137208 cites W2002733845 @default.
• W2912137208 cites W2003279842 @default.
• W2912137208 cites W2003419738 @default.
• W2912137208 cites W2006550061 @default.
• W2912137208 cites W2007700279 @default.
• W2912137208 cites W2007816466 @default.
• W2912137208 cites W2007996045 @default.
• W2912137208 cites W2008456126 @default.
• W2912137208 cites W2009986370 @default.
• W2912137208 cites W2010541697 @default.
• W2912137208 cites W2012819130 @default.
• W2912137208 cites W2014494815 @default.
• W2912137208 cites W2014665449 @default.
• W2912137208 cites W2016223661 @default.
• W2912137208 cites W2019316424 @default.
• W2912137208 cites W2019920565 @default.
• W2912137208 cites W2023213738 @default.
• W2912137208 cites W2024157902 @default.
• W2912137208 cites W2027581094 @default.
• W2912137208 cites W2028764239 @default.
• W2912137208 cites W2028865941 @default.
• W2912137208 cites W2030023077 @default.
• W2912137208 cites W2030432301 @default.
• W2912137208 cites W2030563517 @default.
• W2912137208 cites W2030924263 @default.
• W2912137208 cites W2031192009 @default.
• W2912137208 cites W2033699120 @default.
• W2912137208 cites W2033825289 @default.
• W2912137208 cites W2034445234 @default.
• W2912137208 cites W2034971480 @default.
• W2912137208 cites W2035531827 @default.
• W2912137208 cites W2036210286 @default.
• W2912137208 cites W2036650509 @default.
• W2912137208 cites W2038046442 @default.
• W2912137208 cites W2041602425 @default.
• W2912137208 cites W2044111361 @default.
• W2912137208 cites W2044210746 @default.
• W2912137208 cites W2044753344 @default.
• W2912137208 cites W2045594539 @default.
• W2912137208 cites W2049660991 @default.
• W2912137208 cites W2050333547 @default.
• W2912137208 cites W2052916443 @default.
• W2912137208 cites W2054368497 @default.
• W2912137208 cites W2054631586 @default.
• W2912137208 cites W2054932569 @default.
• W2912137208 cites W2055817459 @default.
• W2912137208 cites W2056038569 @default.
• W2912137208 cites W2056179043 @default.
• W2912137208 cites W2056441884 @default.
• W2912137208 cites W2057863618 @default.
• W2912137208 cites W2063494096 @default.
• W2912137208 cites W2064841659 @default.
• W2912137208 cites W2064893459 @default.
• W2912137208 cites W2065204617 @default.
• W2912137208 cites W2066283966 @default.

• next