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Journal articles on the topic 'Volcanogenic massive sulfide'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Barrie, C. T. "Volcanogenic Massive Sulfide Occurrence Model." Economic Geology 107, no. 5 (2012): 1073. http://dx.doi.org/10.2113/econgeo.107.5.1073.

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2

Vikent’ev, I. V., E. V. Belogub, V. P. Moloshag, and N. I. Eremin. "Selenium in Volcanogenic Massive Sulfide Ores." Doklady Earth Sciences 484, no. 1 (2019): 40–44. http://dx.doi.org/10.1134/s1028334x19010197.

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3

Yang, Kaihui. "Volcanogenic Massive Sulfide Deposits in China." International Geology Review 36, no. 3 (1994): 293–300. http://dx.doi.org/10.1080/00206819409465462.

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4

Dergachev, A. L., and N. I. Eremin. "VOLCANOGENIC MASSIVE SULFIDE DEPOSITS ENRICHED IN GOLD." Moscow University Bulletin. Series 4. Geology, no. 3 (June 28, 2018): 3–11. http://dx.doi.org/10.33623/0579-9406-2018-3-3-11.

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Volcanogenic massive sulfide deposits contain Cu, Zn, Pb, Sb, Bi, Te, Se, Ag, Co and variable amounts of Ag and Au. In some of them gold reserves exceed 100 t while gold grades reach several dozens ppm. Original data base was used to establish statistically meaningful criteria for identification of deposits with large gold reserves and/or anomalously enriched in gold. Some peculiar features of deposits with high Au grades were investigated including distribution in geological history and among the principal metallogenic provinces, association with volcanogenic formations and paleovolcanic stru

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5

Dergachev, A. L., N. I. Eremin, and N. E. Sergeeva. "Volcanogenic massive sulfide deposits of ophiolite associations." Moscow University Geology Bulletin 65, no. 5 (2010): 265–72. http://dx.doi.org/10.3103/s0145875210050017.

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6

Dergachev, A. L., and N. I. Eremin. "Volcanogenic Massive Sulfide Deposits Enriched in Gold." Moscow University Geology Bulletin 73, no. 4 (2018): 325–32. http://dx.doi.org/10.3103/s0145875218040051.

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7

Camprubí, Antoni, Eduardo González-Partida, Lisard Torró, et al. "Mesozoic volcanogenic massive sulfide (VMS) deposits in Mexico." Ore Geology Reviews 81 (March 2017): 1066–83. http://dx.doi.org/10.1016/j.oregeorev.2015.07.027.

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8

Mousivand, Fardin, Ebrahim Rastad, Jan M. Peter, and Sajjad Maghfouri. "Metallogeny of volcanogenic massive sulfide deposits of Iran." Ore Geology Reviews 95 (April 2018): 974–1007. http://dx.doi.org/10.1016/j.oregeorev.2018.01.011.

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9

Mercier-Langevin, Patrick, Mark D. Hannington, Benoît Dubé, and Valérie Bécu. "The gold content of volcanogenic massive sulfide deposits." Mineralium Deposita 46, no. 5-6 (2010): 509–39. http://dx.doi.org/10.1007/s00126-010-0300-0.

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10

Sillitoe, Richard H., Mark D. Hannington, and John F. H. Thompson. "High sulfidation deposits in the volcanogenic massive sulfide environment." Economic Geology 91, no. 1 (1996): 204–12. http://dx.doi.org/10.2113/gsecongeo.91.1.204.

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11

Ohmoto, Hiroshi. "Formation of volcanogenic massive sulfide deposits: The Kuroko perspective." Ore Geology Reviews 10, no. 3-6 (1996): 135–77. http://dx.doi.org/10.1016/0169-1368(95)00021-6.

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12

AVDONIN, Viktor, and Natalia SERGEEVA. "Relics of near-bottom fauna in massive sulfide ores." Domestic geology, no. 3-4 (September 14, 2021): 11–17. http://dx.doi.org/10.47765/0869-7175-2021-10017.

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The additional study of ancient volcanogenic massive sulfide deposits in various regions revealed microtextures, probably of biogenic origin, which could represent varieties of the shells of mineralized fauna. The new finds expand the list of sites containing relics of bioforms associated with hydrothermal vents of "black smokers".

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13

DeMatties, Theodore A. "Early Proterozoic volcanogenic massive sulfide deposits in Wisconsin; an overview." Economic Geology 89, no. 5 (1994): 1122–51. http://dx.doi.org/10.2113/gsecongeo.89.5.1122.

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14

Wyman, D. A. "High‐precision exploration geochemistry: Applications for volcanogenic massive sulfide deposits." Australian Journal of Earth Sciences 47, no. 5 (2000): 861–71. http://dx.doi.org/10.1046/j.1440-0952.2000.00817.x.

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15

Eastoe, C. J., and M. M. Gustin. "Volcanogenic massive sulfide deposits and anoxia in the Phanerozoic oceans." Ore Geology Reviews 10, no. 3-6 (1996): 179–97. http://dx.doi.org/10.1016/0169-1368(95)00022-4.

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16

REVAN, Mustafa Kemal. "Review of Late Cretaceous volcanogenic massive sulfide mineralization in the Eastern Pontides, NE Turkey." TURKISH JOURNAL OF EARTH SCIENCES 29, no. 7 (2020): 1125–53. http://dx.doi.org/10.3906/yer-2006-11.

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The production of Cu-Zn from volcanogenic massive sulfide (VMS) deposits in the eastern Pontides began in the early 1900s, with the exploitation of high-grade ores scattered across the district. The district still possesses economically important blind VMS and associated sulfide deposits. Careful descriptive documentation of the typical features of these VMS ores illustrated the geological characteristics that are important in identifying ore localities and can be used to define exploration targets. The eastern Pontide VMS deposits are examples of volcanic-hosted massive sulfide deposits that

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17

Lalonde, Erik, and Georges Beaudoin. "Petrochemistry, hydrothermal alteration, mineralogy, and sulfur isotope geochemistry of the Turgeon Cu–Zn volcanogenic massive sulfide deposit, northern New Brunswick, Canada." Canadian Journal of Earth Sciences 52, no. 4 (2015): 215–34. http://dx.doi.org/10.1139/cjes-2014-0093.

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The Turgeon deposit is a mafic-type, Cu–Zn volcanogenic massive sulfide (VMS) deposit. It is hosted by Middle Ordovician pillow basalts of the Devereaux Formation of the Fournier Group within the Elmtree-Belledune inlier, near the Bathurst Mining Camp (BMC) in northern New Brunswick, Canada. The Turgeon deposit consists of two Cu–Zn massive sulfide lenses (“100m Zn”, “48-49”) composed of pyrite, chalcopyrite, pyrrhotite, and sphalerite, which are underlain by chalcopyrite–pyrite stockwork veins. Pyrite is overprinted and replaced by chalcopyrite in the stockwork and vent complex sulfide facies

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18

Lindberg, Paul A. "A volcanogenic interpretation for massive sulfide origin, West Shasta District, California." Economic Geology 80, no. 8 (1985): 2240–54. http://dx.doi.org/10.2113/gsecongeo.80.8.2240.

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19

Cagatay, M. Namik. "Hydrothermal alteration associated with volcanogenic massive sulfide deposits; examples from Turkey." Economic Geology 88, no. 3 (1993): 606–21. http://dx.doi.org/10.2113/gsecongeo.88.3.606.

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20

Pan, Yuanming, and Qianli Xie. "EXTREME FRACTIONATION OF PLATINUM GROUP ELEMENTS IN VOLCANOGENIC MASSIVE SULFIDE DEPOSITS." Economic Geology 96, no. 3 (2001): 645–51. http://dx.doi.org/10.2113/gsecongeo.96.3.645.

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21

Bernier, Louis R., and Wallace H. MacLean. "Auriferous chert, banded iron formation, and related volcanogenic hydrothermal alteration, Atik Lake, Manitoba." Canadian Journal of Earth Sciences 26, no. 12 (1989): 2676–90. http://dx.doi.org/10.1139/e89-227.

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Small-scale alteration pipes and stratiform alteration in Archean glomeroporphyritic tholeiitic basalts at Atik Lake, Manitoba, stratigraphically underlie silicate-oxide banded iron formation (BIF) and auriferous sulfide-bearing chert. The auriferous chert is locally interbedded with graphitic argillite, indicating euxinic conditions during deposition. Cordierite–gedrite rocks formed by recrystallization of alteration assemblages during the lower amphibolite-facies metamorphism (T = 550 °C, P = 2.5 kbar). Al2O3, TiO2, Zr, and Nb, which were relatively immobile during alteration, have been used

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22

Torró, Lisard, Joaquín Proenza, Julio Espaillat, et al. "The Discovery of the Romero VMS Deposit and Its Bearing on the Metallogenic Evolution of Hispaniola during the Cretaceous." Minerals 8, no. 11 (2018): 507. http://dx.doi.org/10.3390/min8110507.

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The recently discovered Romero deposit, located in the Tres Palmas district, Cordillera Central of the Dominican Republic, has probable reserves of 840,000 oz gold, 980,000 oz silver and 136 Mlb copper. Mineralization is hosted by intermediate volcanic and volcaniclastic rocks of the lower stratigraphic sequence of the Cretaceous Tireo formation. The andesitic host rocks yield a U-Pb zircon concordia age of 116 ± 10 Ma. Au–Ag–Cu(–Zn) mineralization is divided into: (1) an upper domain with stacked massive sulfide lenses and sulfide dissemination within a 20-m-thick level of massive anhydrite-g

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23

Hou, Zengqian, Shuxian Wang, Andao Du, Xiaoming Qu, and Weidong Sun. "Re-Os Dating of Sulfides from the Volcanogenic Massive Sulfide Deposit at Gacun, Southwestern China." Resource Geology 53, no. 4 (2003): 305–10. http://dx.doi.org/10.1111/j.1751-3928.2003.tb00179.x.

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24

Abraham, S., B. Konka, and S. Gebreselassie. "Geology of volcanogenic massive sulfide deposit near Meli, northwestern Tigray, northern Ethiopia." Momona Ethiopian Journal of Science 7, no. 1 (2015): 85. http://dx.doi.org/10.4314/mejs.v7i1.117239.

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25

White, D. J., C. J. Mwenifumbo, and M. H. Salisbury. "Seismic Properties of Rocks from the Flin Flon Volcanogenic Massive Sulfide Camp." Economic Geology 111, no. 4 (2016): 913–31. http://dx.doi.org/10.2113/econgeo.111.4.913.

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26

Solomon, Michael, and Khin Zaw. "Formation on the sea floor of the Hellyer volcanogenic massive sulfide deposit." Economic Geology 92, no. 6 (1997): 686–95. http://dx.doi.org/10.2113/gsecongeo.92.6.686.

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27

QUERUBIN, Cliff L., and Graciano P. YUMUL. "Stratigraphic Correlation of the Malusok Volcanogenic Massive Sulfide Deposits, Southern Mindanao, Philippines." Resource Geology 51, no. 2 (2001): 135–43. http://dx.doi.org/10.1111/j.1751-3928.2001.tb00087.x.

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28

Rui-Xue, LI, WANG He, XI Zhen-Zhu, et al. "THE 3D TRANSIENT ELECTROMAGNETIC FORWARD MODELING OF VOLCANOGENIC MASSIVE SULFIDE ORE DEPOSITS." Chinese Journal of Geophysics 59, no. 6 (2016): 725–33. http://dx.doi.org/10.1002/cjg2.30020.

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29

Stix, John, Ben Kennedy, Mark Hannington, et al. "Caldera-forming processes and the origin of submarine volcanogenic massive sulfide deposits." Geology 31, no. 4 (2003): 375. http://dx.doi.org/10.1130/0091-7613(2003)031<0375:cfpato>2.0.co;2.

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30

WALKER, J. A., D. R. LENTZ, and S. H. McCLENAGHAN. "The Orvan Brook Volcanogenic Massive Sulfide Deposit: Anatomy of a Highly Attenuated Massive Sulfide System, Bathurst Mining Camp, New Brunswick." Exploration and Mining Geology 15, no. 3-4 (2006): 155–76. http://dx.doi.org/10.2113/gsemg.15.3-4.155.

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31

Almodóvar, Gabriel R., Lola Yesares, Reinaldo Sáez, Manuel Toscano, Felipe González, and Juan Manuel Pons. "Massive Sulfide Ores in the Iberian Pyrite Belt: Mineralogical and Textural Evolution." Minerals 9, no. 11 (2019): 653. http://dx.doi.org/10.3390/min9110653.

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The Iberian Pyrite Belt (IPB) is recognized as having one of the major concentrations of volcanogenic massive sulfide (VMS) deposits on Earth. Original resources of about 2000 Mt of massive sulfides have been reported in the province. Recent classifications have considered the IPB deposits as the bimodal siliciclastic subtype, although major differences can be recognized among them. The main ones concern the hosting rocks. To the north, volcanic and volcaniclastic depositional environments predominate, whereas to the south, black shale-hosted VMS prevail. The mineral composition is quite simpl

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32

Ioannou, S. E., E. T. C. Spooner, and C. T. Barrie. "Fluid Temperature and Salinity Characteristics of the Matagami Volcanogenic Massive Sulfide District, Quebec." Economic Geology 102, no. 4 (2007): 691–715. http://dx.doi.org/10.2113/gsecongeo.102.4.691.

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33

Halley, S. W., and R. H. Roberts. "Henty; a shallow-water gold-rich volcanogenic massive sulfide deposit in western Tasmania." Economic Geology 92, no. 4 (1997): 438–47. http://dx.doi.org/10.2113/gsecongeo.92.4.438.

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34

Yakushi, Daigoro, and Mamoru Enjoji. "Chemical Composition of Ores from the Takara Volcanogenic Massive Sulfide Deposit, Central Japan." Resource Geology 54, no. 4 (2004): 437–46. http://dx.doi.org/10.1111/j.1751-3928.2004.tb00219.x.

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35

Wang, Changming, Jun Deng, Shouting Zhang, and Liqiang Yang. "Metallogenic Province and Large Scale Mineralization of Volcanogenic Massive Sulfide Deposits in China." Resource Geology 60, no. 4 (2010): 404–13. http://dx.doi.org/10.1111/j.1751-3928.2010.00127.x.

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36

Kuzebnyy, V. S., Ye A. Kaleyev, and V. A. Makarov. "VOLCANOGENIC-SEDIMENTARY MASSIVE SULFIDE MINERALIZATION OF THE KYZYL-TASHTYG ORE FIELD, EASTERN TUVA." International Geology Review 32, no. 4 (1990): 384–90. http://dx.doi.org/10.1080/00206819009465785.

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37

Cathles, Lawrence M. "What processes at mid-ocean ridges tell us about volcanogenic massive sulfide deposits." Mineralium Deposita 46, no. 5-6 (2010): 639–57. http://dx.doi.org/10.1007/s00126-010-0292-9.

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38

Saunders, James A., and Gilles O. Allard. "The Scott Lake deposit: a contact-metamorphosed volcanogenic massive sulfide deposit, Chibougamau area, Quebec." Canadian Journal of Earth Sciences 27, no. 2 (1990): 180–86. http://dx.doi.org/10.1139/e90-018.

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The Scott Lake volcanogenic massive sulfide deposit lies near the margin of a large, early kinematic granitoid intrusion in the vicinity of Chibougamau, Quebec. The deposit was contact metamorphosed by the intrusion, and subsequently it was metamorphosed to the greenschist facies during the Kenoran Orogeny. Pyrite, magnetite, and sphalerite are the most abundant metallic minerals, and minor amounts of chalcopyrite, pyrrhotite, and loellingite are also present. Both pyrite and magnetite locally occur as porphyroblasts up to several centimetres in diameter. Metamorphic textures developed in the

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39

SERAVINA, Tatyana, Svetlana KUZNETSOVA, and Ludmila FILATOVA. "Compositional peculiarities of the host rocks and ores of the Lazursky ore field, Zmeinogorsk ore region of the Rudny Altai minerogenic zone." Domestic geology, no. 3-4 (September 14, 2021): 36–47. http://dx.doi.org/10.47765/0869-7175-2021-10020.

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The article describes composition of the host rocks and ores of the Lazursky and Maslyansky polymetallic volcanogenic massive sulfide deposits of the Lazursky ore field located within the Zmeinogorsk ore region of the Rudny Altai minerogenic zone. The ore field is composed of various facies of the Devonian (Late Givetian – Frasnian) ore-bearing siliceous-terrigenous basalt-rhyolite formation containing horizons of synvolcanic metasomatites. All rocks of the ore field were subjected to folding and schistosity with zones of tectonic brecciation. Hydrothermal alterations are represented by carbon

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40

Vallée, Marc A., Richard S. Smith, and Pierre Keating. "Case history of combined airborne time-domain electromagnetics and power-line field survey in Chibougamau, Canada." GEOPHYSICS 75, no. 2 (2010): B67—B72. http://dx.doi.org/10.1190/1.3343573.

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Exploration for volcanogenic massive sulfides requires good geologic understanding. Geologic knowledge often is limited by a lack of outcrops. This is especially true in Canada under residual glacial covers. Geologic information must therefore be complemented by information obtained using means such as geophysical and geochemical observations. Electromagnetic (EM) methods extend lithological understanding to depths beyond the overburden. Massive sulfides are highly conductive and, depending on their depth and volume, may be detected easily by airborne EM surveys. They are more often equant tha

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41

Yartsev, E. I., I. V. Vikentyev та V. Yu Prokofiev. "Mineralogical and geochemical evidenceof contact transformation of Dzhusа base metal massive sulfide deposit (South Urals)". Moscow University Bulletin. Series 4. Geology, № 1 (28 лютого 2017): 39–44. http://dx.doi.org/10.33623/0579-9406-2017-1-39-44.

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Dzhusа volcanogenic massive sulfide deposit is characterized by a high concentration of dykes of basic and intermediate rocks. Thermal metamorphism of ore and recrystallization of ore minerals were caused by formation of post-ore dykes. It was shown that homogenization temperature regular increased from 156 °С at a distance of the dyke to 287-305 °С in its contact zone. Highly saline (6,4-15,7 wt.% eq. NaCl) water fluids saturated with CO2 suggest high pres- sure conditions (up to 1500 bars) and can result from contact and regional metamorphism.

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42

Pehrsson, Sally, Harold L. Gibson, and Kelly Gilmore. "A Special Issue on Volcanogenic Massive Sulfide Deposits of the Trans-Hudson Orogen: Preface." Economic Geology 111, no. 4 (2016): 803–16. http://dx.doi.org/10.2113/econgeo.111.4.803.

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43

Schmidt, Jeanine M. "Stratigraphic setting and mineralogy of the Arctic volcanogenic massive sulfide prospect, Ambler District, Alaska." Economic Geology 81, no. 7 (1986): 1619–43. http://dx.doi.org/10.2113/gsecongeo.81.7.1619.

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44

Gemmell, J. Bruce, and Ross R. Large. "Stringer system and alteration zones underlying the Hellyer volcanogenic massive sulfide deposit, Tasmania, Australia." Economic Geology 87, no. 3 (1992): 620–49. http://dx.doi.org/10.2113/gsecongeo.87.3.620.

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45

Syme, E. C., and A. H. Bailes. "Stratigraphic and tectonic setting of early Proterozoic volcanogenic massive sulfide deposits, Flin Flon, Manitoba." Economic Geology 88, no. 3 (1993): 566–89. http://dx.doi.org/10.2113/gsecongeo.88.3.566.

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46

Brauhart, Carl W., David I. Groves, and Peter Morant. "Regional alteration systems associated with volcanogenic massive sulfide mineralization at Panorama, Pilbara, Western Australia." Economic Geology 93, no. 3 (1998): 292–302. http://dx.doi.org/10.2113/gsecongeo.93.3.292.

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47

Hassan, Lee Y., and Malcolm P. Roberts. "Tellurides associated with volcanogenic massive sulfide (VMS) mineralization at Yuinmery and Austin, Western Australia." Ore Geology Reviews 80 (January 2017): 352–62. http://dx.doi.org/10.1016/j.oregeorev.2016.07.005.

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48

Dergachev, A. L., and N. I. Eremin. "Volcanogenic massive sulfide and sedimentary-exhalation lead-zinc ore formation during the Earth’s history." Doklady Earth Sciences 423, no. 1 (2008): 1220–22. http://dx.doi.org/10.1134/s1028334x08080084.

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49

Barrie, C. Tucker, Craig Taylor, and Doreen E. Ames. "Geology and Metal Contents of the Ruttan volcanogenic massive sulfide deposit, northern Manitoba, Canada." Mineralium Deposita 39, no. 8 (2005): 795–812. http://dx.doi.org/10.1007/s00126-004-0455-7.

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50

Barrie, C. Tucker, Craig Taylor, and Doreen E. Ames. "Geology and metal contents of the Ruttan volcanogenic massive sulfide deposit, northern Manitoba, Canada." Mineralium Deposita 41, no. 8 (2006): 837. http://dx.doi.org/10.1007/s00126-006-0087-1.

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