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• W2766131656 endingPage "671" @default.
• W2766131656 startingPage "656" @default.
• W2766131656 abstract "Abstract PYRITE is ubiquitous throughout the massive sulfide deposits of the Bathurst Mining Camp, Canada. Pyrite locally preserves primary, pseudo-primary textures, as well as secondary textures, that formed in response to the hydrothermal, metamorphic, and deformation processes to which the host sequence was exposed. In the Bathurst Mining Camp most forms of pyrite are arsenian (up to 3.13 wt% As), with considerable enrichment in Tl, Sb, Sn, Bi, Ag, Se, and to a lesser extent Cd, Ga, Te, Hg, Ge, In, and Au. LA-ICP-MS analyses of primary pyrite show significant enrichment in fluid-mobile elements, in particular, Tl, Sb, As, and Hg, as well as Bi, Pb, and Sn. In contrast, secondary pyrite (syn-to post-deformation varieties) is not enriched in these elements. Superimposed metamorphism typically causes loss of fluid-mobile elements to different degrees, except for Se. Pyrite chemical variations have the potential to monitor ore petrogenesis at inter- and intra-deposit scales. Pyrite from the Cu-zone is enriched in Se relative to pyrite from Zn-Pb zone, in which Tl is elevated. Throughout the host sequence fluid-mobile element concentrations of pyrite vary by several orders magnitude, with the highest fluid-mobile element abundances in footwall rocks immediately proximal to the deposit. Moreover, elevated fluid-mobile element concentrations of pyrite are recognized in footwall felsic volcanic and sedimentary rocks as much as several hundred metres away from the deposit. Hanging-wall zones contain pyrite with fluid-mobile element contents comparable to pyrite from sulfide horizon. The fluid-mobile element concentrations of pyrite are higher in exhalative sedimentary rocks than pyrite from the sulfide mineralization itself. The spatial variation in fluid-mobile element concentrations in pyrite as identified using LA-ICP-MS can be used to identify otherwise cryptic deposit-related haloes. Ultimately, this technique, when combined with traditional exploration tools, can be used to vector toward VMS mineralization in the Bathurst Mining Camp and possibly a useful indicator in a prospect-scale base metal exploration." @default.
• W2766131656 created "2017-11-10" @default.
• W2766131656 creator A5015800779 @default.
• W2766131656 creator A5044404954 @default.
• W2766131656 creator A5057707874 @default.
• W2766131656 creator A5080721488 @default.
• W2766131656 date "2018-01-01" @default.
• W2766131656 modified "2023-10-12" @default.
• W2766131656 title "Assessment of pyrite composition by LA-ICP-MS techniques from massive sulfide deposits of the Bathurst Mining Camp, Canada: From textural and chemical evolution to its application as a vectoring tool for the exploration of VMS deposits" @default.
• W2766131656 cites W1434692241 @default.
• W2766131656 cites W1964704563 @default.
• W2766131656 cites W1965375933 @default.
• W2766131656 cites W1965744338 @default.
• W2766131656 cites W1967780504 @default.
• W2766131656 cites W1968868266 @default.
• W2766131656 cites W1969023317 @default.
• W2766131656 cites W1969725957 @default.
• W2766131656 cites W1969954382 @default.
• W2766131656 cites W1975256512 @default.
• W2766131656 cites W1976550881 @default.
• W2766131656 cites W1976819346 @default.
• W2766131656 cites W1977639716 @default.
• W2766131656 cites W1979727721 @default.
• W2766131656 cites W1982002946 @default.
• W2766131656 cites W1989872055 @default.
• W2766131656 cites W1989989545 @default.
• W2766131656 cites W1992614560 @default.
• W2766131656 cites W1996094090 @default.
• W2766131656 cites W1997337532 @default.
• W2766131656 cites W1998048740 @default.
• W2766131656 cites W2001201232 @default.
• W2766131656 cites W2002254031 @default.
• W2766131656 cites W2005877813 @default.
• W2766131656 cites W2010802388 @default.
• W2766131656 cites W2013358099 @default.
• W2766131656 cites W2013617247 @default.
• W2766131656 cites W2015711821 @default.
• W2766131656 cites W2018093298 @default.
• W2766131656 cites W2019501187 @default.
• W2766131656 cites W2025203052 @default.
• W2766131656 cites W2029567205 @default.
• W2766131656 cites W2031605041 @default.
• W2766131656 cites W2033768654 @default.
• W2766131656 cites W2036544042 @default.
• W2766131656 cites W2037193039 @default.
• W2766131656 cites W2039649774 @default.
• W2766131656 cites W2042795036 @default.
• W2766131656 cites W2044407876 @default.
• W2766131656 cites W2046500701 @default.
• W2766131656 cites W2046903318 @default.
• W2766131656 cites W2046907778 @default.
• W2766131656 cites W2051269194 @default.
• W2766131656 cites W2051323905 @default.
• W2766131656 cites W2052210533 @default.
• W2766131656 cites W2055142051 @default.
• W2766131656 cites W2056228634 @default.
• W2766131656 cites W2059058479 @default.
• W2766131656 cites W2060128531 @default.
• W2766131656 cites W2061590669 @default.
• W2766131656 cites W2061881401 @default.
• W2766131656 cites W2063207193 @default.
• W2766131656 cites W2064275717 @default.
• W2766131656 cites W2064760651 @default.
• W2766131656 cites W2069894760 @default.
• W2766131656 cites W2074330508 @default.
• W2766131656 cites W2077266669 @default.
• W2766131656 cites W2083960283 @default.
• W2766131656 cites W2087532394 @default.
• W2766131656 cites W2088096040 @default.
• W2766131656 cites W2090143505 @default.
• W2766131656 cites W2091893799 @default.
• W2766131656 cites W2092156812 @default.
• W2766131656 cites W2100191999 @default.
• W2766131656 cites W2101108033 @default.
• W2766131656 cites W2102727961 @default.
• W2766131656 cites W2104955145 @default.
• W2766131656 cites W2105163101 @default.
• W2766131656 cites W2114955000 @default.
• W2766131656 cites W2116756045 @default.
• W2766131656 cites W2119786876 @default.
• W2766131656 cites W2122079174 @default.
• W2766131656 cites W2122783351 @default.
• W2766131656 cites W2127127146 @default.
• W2766131656 cites W2130626244 @default.
• W2766131656 cites W2132280939 @default.
• W2766131656 cites W2136080405 @default.
• W2766131656 cites W2139678104 @default.
• W2766131656 cites W2146169543 @default.
• W2766131656 cites W2153000470 @default.
• W2766131656 cites W2154295153 @default.
• W2766131656 cites W2154499471 @default.
• W2766131656 cites W2154506653 @default.
• W2766131656 cites W2159347349 @default.
• W2766131656 cites W2161188057 @default.
• W2766131656 cites W2170575916 @default.
• W2766131656 cites W2202490468 @default.
• W2766131656 cites W2231608875 @default.
• W2766131656 cites W2305524422 @default.

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