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Journal articles on the topic 'Seafloor massive sulfide'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 January 2023

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1

Firstova, Anna, Georgy Cherkashov, Tamara Stepanova, Anna Sukhanova, Irina Poroshina, and Victor Bel’tenev. "New Data for the Internal Structure of Ultramafic Hosted Seafloor Massive Sulfides (SMS) Deposits: Case Study of the Semenov-5 Hydrothermal Field (13°31′ N, MAR)." Minerals 12, no. 12 (2022): 1593. http://dx.doi.org/10.3390/min12121593.

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The internal structure of Seafloor Massive Sulfides (SMS) deposits is one of the most important and complex issues facing the study of modern hydrothermal ore systems. The Semenov-5 hydrothermal field is a unique area where mass wasting on the slope of the oceanic core complex (OCC) structure exposes the subsurface portion of the deposit and offers an exceptional opportunity to observe massive sulfides that have formed not only on the seafloor but in sub-seafloor zones as well. This paper examines the internal structure of the OCC-related Semenov-5 hydrothermal field along with analysis of the

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2

Wu, Caowei, Changchun Zou, Cheng Peng, et al. "Numerical Simulation Study on the Relationships between Mineralized Structures and Induced Polarization Properties of Seafloor Polymetallic Sulfide Rocks." Minerals 12, no. 9 (2022): 1172. http://dx.doi.org/10.3390/min12091172.

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The induced polarization (IP) method plays an important role in the detection of seafloor polymetallic sulfide deposits. Numerical simulations based on the Poisson–Nernst–Planck equation and the Maxwell equation were performed. The effects of mineralized structures on the IP and electrical conductivity properties of seafloor sulfide-bearing rocks were investigated. The results show that total chargeability increases linearly as the volume content of disseminated metal sulfides increases when the volume content is below 20%. However, total chargeability increases nonlinearly with increasing vol

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3

Anderson, Melissa O., Mark D. Hannington, Timothy F. McConachy, et al. "Mineralization and Alteration of a Modern Seafloor Massive Sulfide Deposit Hosted in Mafic Volcaniclastic Rocks." Economic Geology 114, no. 5 (2019): 857–96. http://dx.doi.org/10.5382/econgeo.4666.

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Abstract Tinakula is the first seafloor massive sulfide deposit described in the Jean Charcot troughs and is the first such deposit described in the Solomon Islands—on land or the seabed. The deposit is hosted by mafic (basaltic-andesitic) volcaniclastic rocks within a series of cinder cones along a single eruptive fissure. Extensive mapping and sampling by remotely operated vehicle, together with shallow drilling, provide insights into deposit geology and especially hydrothermal processes operating in the shallow subsurface. On the seafloor, mostly inactive chimneys and mounds cover an area o

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4

Liu, Lushi, Jilong Lu, Chunhui Tao, and Shili Liao. "Prospectivity Mapping for Magmatic-Related Seafloor Massive Sulfide on the Mid-Atlantic Ridge Applying Weights-of-Evidence Method Based on GIS." Minerals 11, no. 1 (2021): 83. http://dx.doi.org/10.3390/min11010083.

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The Mid-Atlantic Ridge belongs to slow-spreading ridges. Hannington predicted that there were a large number of mineral resources on slow-spreading ridges; however, seafloor massive sulfide deposits usually develop thousands of meters below the seafloor, which make them extremely difficult to explore. Therefore, it is necessary to use mineral prospectivity mapping to narrow the exploration scope and improve exploration efficiency. Recently, Fang and Shao conducted mineral prospectivity mapping of seafloor massive sulfide on the northern Mid-Atlantic Ridge, but the mineral prospectivity mapping

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5

GABLINA, IRINA. "Role of geochemical barriers in forming sulfide ores in various geological environments." Domestic geology, no. 2 (May 27, 2021): 63–73. http://dx.doi.org/10.47765/0869-7175-2021-10014.

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Based on long-term studies of cupriferous sandstone and shale deposits, as well as deepsea sulfide ores, various types of geochemical barriers where sulfides form are shown. Cupriferous sandstones and shales form as metals precipitate from redbed reservoir waters on H2S geochemical barrier. Syngenetic and epigenetic barrier types are identified. Oceanic sulfide ores from the Central Atlantic region were studied; as a result, a new hydrothermal-metasomatic sediment-hosted mineralization type was found, along with previously known sulfide ore types (massive ores on the seafloor and stockwork ore

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6

Hannington, M., J. Jamieson, T. Monecke, S. Petersen, and S. Beaulieu. "The abundance of seafloor massive sulfide deposits." Geology 39, no. 12 (2011): 1155–58. http://dx.doi.org/10.1130/g32468.1.

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7

Tseluyko, A. S., V. V. Maslennikov, N. R. Aupova, and S. P. Maslennikova. "Mineral and textural-structural features of the ore facies of Yubileynoye massive sulfide deposit (the Southern Urals)." Proceedings of higher educational establishments. Geology and Exploration, no. 4 (August 28, 2017): 50–56. http://dx.doi.org/10.32454/0016-7762-2017-4-50-56.

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A study of the ore facies of the massive sulfide ores from the Yubileynoe deposit (ore body № 2) has been shown. The sub-seafloor and seafloor hydrothermal, biogenic, clastic and seafloor hypergenic facies have been diagnosed in the studied ores, reflecting different formation conditions within the ore body № 2. The seafloor and sub-seafloor hydrothermal facies occur in the central part of the ore body, while clastic with seafloor hypergenic facies dominate at the flanks of the ore body. Rare minerals are native gold, minerals of Ag, Te, Bi and Pb widespread in seafloor hydrothermal and clasti

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8

Hu, Jianhua, Shaojun Liu, and Ruiqiang Zhang. "A New Exploitation Tool of Seafloor Massive Sulfide." Thalassas: An International Journal of Marine Sciences 32, no. 2 (2016): 101–4. http://dx.doi.org/10.1007/s41208-016-0014-x.

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9

Fuchs, Sebastian, Mark D. Hannington, and Sven Petersen. "Divining gold in seafloor polymetallic massive sulfide systems." Mineralium Deposita 54, no. 6 (2019): 789–820. http://dx.doi.org/10.1007/s00126-019-00895-3.

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10

Jamieson, J. W., and A. Gartman. "Defining active, inactive, and extinct seafloor massive sulfide deposits." Marine Policy 117 (July 2020): 103926. http://dx.doi.org/10.1016/j.marpol.2020.103926.

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11

Safipour, Roxana, Sebastian Hölz, Jesse Halbach, Marion Jegen, Sven Petersen, and Andrei Swidinsky. "A self-potential investigation of submarine massive sulfides: Palinuro Seamount, Tyrrhenian Sea." GEOPHYSICS 82, no. 6 (2017): A51—A56. http://dx.doi.org/10.1190/geo2017-0237.1.

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The self-potential (SP) method detects naturally occurring electric fields, which may be produced by electrically conductive mineral deposits, such as massive sulfides. Recently, there has been increasing interest in applying this method in a marine environment to explore for seafloor massive sulfide (SMS) deposits, which may contain economic resources of base and precious metals. Although SMS sites that are associated with active venting and are not buried under sediment cover are known to produce an SP signal, the effectiveness of the method at detecting inactive and sediment-covered deposit

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12

Singer, Donald A. "Base and precious metal resources in seafloor massive sulfide deposits." Ore Geology Reviews 59 (June 2014): 66–72. http://dx.doi.org/10.1016/j.oregeorev.2013.11.008.

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13

Lehrmann, Berit, Iain Stobbs, Paul Lusty, and Bramley Murton. "Insights into Extinct Seafloor Massive Sulfide Mounds at the TAG, Mid-Atlantic Ridge." Minerals 8, no. 7 (2018): 302. http://dx.doi.org/10.3390/min8070302.

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Over the last decade there has been an increasing interest in deep-sea mineral resources that may contribute to future raw metal supply. However, before seafloor massive sulfides (SMS) can be considered as a resource, alteration and weathering processes that may affect their metal tenor have to be fully understood. This knowledge cannot be obtained by assessing the surface exposures alone. Seafloor drilling is required to gain information about the third dimension. In 2016, three extinct seafloor massive sulfide mounds, located in the Trans-Atlantic Geotraverse (TAG) hydrothermal area of the M

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14

Maslennikov, Valeriy V., Nuriya R. Ayupova, Nataliya P. Safina, et al. "Mineralogical Features of Ore Diagenites in the Urals Massive Sulfide Deposits, Russia." Minerals 9, no. 3 (2019): 150. http://dx.doi.org/10.3390/min9030150.

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In weakly metamorphosed massive sulfide deposits of the Urals (Dergamysh, Yubileynoe, Yaman-Kasy, Molodezhnoe, Valentorskoe, Aleksandrinskoe, Saf’yanovskoe), banded sulfides (ore diagenites) are recognized as the products of seafloor supergene alteration (halmyrolysis) of fine-clastic sulfide sediments and further diagenesis leading to the formation of authigenic mineralization. The ore diagenites are subdivided into pyrrhotite-, chalcopyrite-, bornite-, sphalerite-, barite- and hematite-rich types. The relative contents of sphalerite-, bornite- and barite-rich facies increases in the progress

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15

Liu, Shaojun, Jianhua Hu, Ruiqiang Zhang, Yu Dai, and Hengling Yang. "Development of mining technology and equipment for seafloor massive sulfide deposits." Chinese Journal of Mechanical Engineering 29, no. 5 (2016): 863–70. http://dx.doi.org/10.3901/cjme.2016.0815.093.

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16

Cherkashov, G. A., V. N. Ivanov, V. I. Bel’tenev, et al. "Seafloor Massive Sulfide Deposits of the Northern Equatorial Mid-Atlantic Ridge." Океанология 53, no. 5 (2013): 680–93. http://dx.doi.org/10.7868/s0030157413050031.

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17

Maslennikov, Valeriy, Georgy Cherkashov, Dmitry Artemyev, et al. "Pyrite Varieties at Pobeda Hydrothermal Fields, Mid-Atlantic Ridge 17°07′–17°08′ N: LA-ICP-MS Data Deciphering." Minerals 10, no. 7 (2020): 622. http://dx.doi.org/10.3390/min10070622.

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The massive sulfide ores of the Pobeda hydrothermal fields are grouped into five main mineral microfacies: (1) isocubanite-pyrite, (2) pyrite-wurtzite-isocubanite, (3) pyrite with minor isocubanite and wurtzite-sphalerite microinclusions, (4) pyrite-rich with framboidal pyrite, and (5) marcasite-pyrite. This sequence reflects the transition from feeder zone facies to seafloor diffuser facies. Spongy, framboidal, and fine-grained pyrite varieties replaced pyrrhotite, greigite, and mackinawite “precursors”. The later coarse and fine banding oscillatory-zoned pyrite and marcasite crystals are ove

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18

Li, Yan, Meng-Dan Li, Huan Dai, and Ke-Sen Liang. "Study on Cutting-Load Characteristics of Collecting Cutter for Seafloor Massive Sulfide." IEEE Access 9 (2021): 51925–39. http://dx.doi.org/10.1109/access.2021.3070007.

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19

Park, Se-Hun, Seong-Wook Park, and Suk-Jae Kwon. "Development of Technical and Economic Evaluation Model for Seafloor Massive Sulfide Deposits." Ocean and Polar Research 28, no. 2 (2006): 187–99. http://dx.doi.org/10.4217/opr.2006.28.2.187.

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20

Peng, Ronghua, Bo Han, and Xiangyun Hu. "Exploration of Seafloor Massive Sulfide Deposits with Fixed-Offset Marine Controlled Source Electromagnetic Method: Numerical Simulations and the Effects of Electrical Anisotropy." Minerals 10, no. 5 (2020): 457. http://dx.doi.org/10.3390/min10050457.

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Seafloor massive sulfide (SMS) deposits have attracted growing interest and become the focus of current seafloor mineral exploration. One key challenge is to delineate potential SMS accumulations and estimate their quantity and quality for prospective resource mining. Recently, geophysical electromagnetic methods which are routinely used for land-based mineral exploration are being adapted to detect and assess SMS occurrences by imaging their conductivity distributions. However, the rough seafloor topography and electrical anisotropy of the seafloor formations encountered in practical surveys

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21

Kasashima, Yuki, and Shigeru Tabeta. "A Study on the Social Acceptance for the Development of Seafloor Massive Sulfide." Journal of the Japan Society of Naval Architects and Ocean Engineers 15 (2012): 167–74. http://dx.doi.org/10.2534/jjasnaoe.15.167.

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22

Tabeta, Shigeru, and Yuki Kasashima. "Assessment of business feasibility for the development of seafloor massive sulfide considering uncertainty." Journal of the Japan Society of Naval Architects and Ocean Engineers 17 (2013): 143–48. http://dx.doi.org/10.2534/jjasnaoe.17.143.

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23

Kubota, Ryuji, Hidehiro Ishikawa, Chikara Okada, Takeya Matsuda, and Yutaka Kanai. "Marine deep-towed self-potential and DC resistivity explorations for seafloor massive sulfide deposits." BUTSURI-TANSA(Geophysical Exploration) 73 (2020): 3–13. http://dx.doi.org/10.3124/segj.73.3.

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24

Boschen, RE, AA Rowden, MR Clark, SJ Barton, A. Pallentin, and JPA Gardner. "Megabenthic assemblage structure on three New Zealand seamounts: implications for seafloor massive sulfide mining." Marine Ecology Progress Series 523 (March 16, 2015): 1–14. http://dx.doi.org/10.3354/meps11239.

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25

Tara, Kenji, and Nobuo Kawai. "Development of the exploration method and integrated interpretation tool for Seafloor Massive Sulfide（SMS）." Journal of the Japanese Association for Petroleum Technology 84, no. 1 (2019): 85–89. http://dx.doi.org/10.3720/japt.84.85.

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26

Boschen, Rachel E., Ashley A. Rowden, Malcolm R. Clark, Arne Pallentin, and Jonathan P. A. Gardner. "Seafloor massive sulfide deposits support unique megafaunal assemblages: Implications for seabed mining and conservation." Marine Environmental Research 115 (April 2016): 78–88. http://dx.doi.org/10.1016/j.marenvres.2016.02.005.

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27

Collins, Patrick Colman, Peter Croot, Jens Carlsson, et al. "A primer for the Environmental Impact Assessment of mining at seafloor massive sulfide deposits." Marine Policy 42 (November 2013): 198–209. http://dx.doi.org/10.1016/j.marpol.2013.01.020.

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28

Ishizu, K., T. Goto, Y. Ohta, et al. "Internal Structure of a Seafloor Massive Sulfide Deposit by Electrical Resistivity Tomography, Okinawa Trough." Geophysical Research Letters 46, no. 20 (2019): 11025–34. http://dx.doi.org/10.1029/2019gl083749.

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29

Novoselov, K. A., E. V. Belogub, S. A. Sadykov, and I. V. Vikentyev. "Gossan of the Yubileynoe massive sulfide deposit (South Urals): evidence for formation on the seafloor." Литология и полезные ископаемые 1, no. 1 (2019): 90–100. http://dx.doi.org/10.31857/s0024-497x2019190-100.

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Oxidation zone of the Yubileinoe massive sulfide deposit, South Urals, is buried beneath Jurassic sediments containing coalified plant remains. Mineralogy of gossan of this deposit is marked by the abundance of siderite. The carbon isotope composition (δ13C) in siderite varies from -20.0 to -23.4‰ PDB, which is close to δ13C variation in coals from the overlying sediments (-23.5 to -26.2‰ PDB). The formation of siderite is likely related to interaction between solutions of the Triassic oxidation zone and fermentation products of the organic matter.

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30

Ishibashi, Jun-ichiro, and Tetsuro Urabe. "Geoscientific model of a seafloor hydrothermal system associated with the formation of massive sulfide deposits." BUTSURI-TANSA(Geophysical Exploration) 73 (2020): 74–82. http://dx.doi.org/10.3124/segj.73.74.

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31

MONECKE, Thomas, and Patrick MERCIER-LANGEVIN. "Gold in the Massive Sulfide Environment: A Comparison of Ancient and Modern Seafloor Hydrothermal Systems." Acta Geologica Sinica - English Edition 88, s2 (2014): 190–91. http://dx.doi.org/10.1111/1755-6724.12369_23.

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32

Gartman, Amy, Samantha P. Whisman, and James R. Hein. "Sphalerite Oxidation in Seawater with Covellite: Implications for Seafloor Massive Sulfide Deposits and Mine Waste." ACS Earth and Space Chemistry 4, no. 12 (2020): 2261–69. http://dx.doi.org/10.1021/acsearthspacechem.0c00177.

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33

Novoselov, K. A., E. V. Belogub, S. A. Sadykov, and I. V. Vikentyev. "Gossan of the Yubileinoe Massive Sulfide Deposit (South Urals): Evidence for Formation on the Seafloor." Lithology and Mineral Resources 54, no. 1 (2019): 66–78. http://dx.doi.org/10.1134/s002449021901005x.

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34

Tseluyko, A. S., V. V. Maslennikov, N. R. Ayupova, S. P. Maslennikova, and L. V. Danyushevsky. "Tellurium-bearing minerals in clastic ores of Ybileynoe massive sulfide deposit (South Urals)." Геология рудных месторождений 61, no. 2 (2019): 39–71. http://dx.doi.org/10.31857/s0016-777061239-71.

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At the well preserved Yubileynoe VMS deposit (South Urals), sulfide breccias and turbidites contain abundant tellurides represented by hessite, coloradoite, altaite, volynskite, stutzite, petzite, calaverite as well as phases of intermediate solid solution tellurobismuthite – rucklidgeite. There is three generation of tellurides were highlighted: 1) primary hydrothermal tellurides in the fragments of chalcopyrite and sphalerite of chalcopyrite-rich black smoker chimneys; 2) authigenic tellurides in pseudomorphic chalcopyrite and veins of chalcopyrite after fragments of colloform and granular p

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35

Spagnoli, Giovanni, Andreas Jahn, and Peter Halbach. "First results regarding the influence of mineralogy on the mechanical properties of seafloor massive sulfide samples." Engineering Geology 214 (November 2016): 127–35. http://dx.doi.org/10.1016/j.enggeo.2016.10.007.

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36

Kato, Shingo, Kei Ikehata, Takazo Shibuya, Tetsuro Urabe, Moriya Ohkuma, and Akihiko Yamagishi. "Potential for biogeochemical cycling of sulfur, iron and carbon within massive sulfide deposits below the seafloor." Environmental Microbiology 17, no. 5 (2014): 1817–35. http://dx.doi.org/10.1111/1462-2920.12648.

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37

Juliani, Cyril, and Steinar Løve Ellefmo. "Multi-scale Quantitative Risk Analysis of Seabed Minerals: Principles and Application to Seafloor Massive Sulfide Prospects." Natural Resources Research 28, no. 3 (2018): 909–30. http://dx.doi.org/10.1007/s11053-018-9427-y.

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38

Kim Cawood, Tarryn, and Abraham Rozendaal. "A Multistage Genetic Model for the Metamorphosed Mesoproterozoic Swartberg Base Metal Deposit, Aggeneys-Gamsberg Ore District, South Africa." Economic Geology 115, no. 5 (2020): 1021–54. http://dx.doi.org/10.5382/econgeo.4725.

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Abstract The polymetamorphosed Swartberg Cu-Pb-Zn-Ag deposit in the Namaqua Metamorphic Province of South Africa is a major metal producer in the region, yet its genesis remains poorly understood. The deposit comprises several stratiform to stratabound units, namely the Lower Orebody and Dark Quartzite, the overlying Barite Unit, and the Upper Orebody, all of which are folded by an F2 isoclinal syncline and refolded by an open F3 synform. A discordant Garnet Quartzite unit surrounds the Upper Orebody in the F2 hinge, where it overprints the Lower Orebody and Barite Unit. The Lower Orebody comp

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39

Diehl, Alexander, Cornel E. J. de Ronde, and Wolfgang Bach. "Subcritical Phase Separation and Occurrence of Deep-Seated Brines at the NW Caldera Vent Field, Brothers Volcano: Evidence from Fluid Inclusions in Hydrothermal Precipitates." Geofluids 2020 (September 16, 2020): 1–22. http://dx.doi.org/10.1155/2020/8868259.

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The northwestern caldera wall of Brothers volcano in the southern Kermadec arc features several clusters of hydrothermal venting in a large area that extends from near the caldera floor (~1700 mbsl) almost up to the crater rim (~1300 mbsl). Abundant black smoker-type hydrothermal chimneys and exposed stockwork mineralization in this area provide an excellent archive of hydrothermal processes that form seafloor massive sulfide deposits. Using sulfate precipitates from chimneys and stockwork recently recovered by remotely operated vehicles, we conducted fluid inclusion microthermometry and Sr is

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40

Fallon, Emily, Matthias Frische, Sven Petersen, Richard Brooker, and Thomas Scott. "Geological, Mineralogical and Textural Impacts on the Distribution of Environmentally Toxic Trace Elements in Seafloor Massive Sulfide Occurrences." Minerals 9, no. 3 (2019): 162. http://dx.doi.org/10.3390/min9030162.

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With mining of seafloor massive sulfides (SMS) coming closer to reality, it is vital that we have a good understanding of the geochemistry of these occurrences and the potential toxicity impact associated with mining them. In this study, SMS samples from seven hydrothermal fields from various tectonic settings were investigated by in-situ microanalysis (electron microprobe (EMPA) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS)) to highlight the distribution of potentially-toxic trace elements (Cu, Zn, Pb, Mn, Cd, As, Sb, Co, Ni, Bi, Ag and Hg) within the deposits, t

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41

Ishizu, Keiichi, Chatchai Vachiratienchai, Weerachai Siripunvaraporn, Tada-nori Goto, Takafumi Kasaya, and Hisanori Iwamoto. "Evaluations of effectiveness of marine deep-towed DC resistivity survey in investigation of seafloor massive sulfide deposits." BUTSURI-TANSA(Geophysical Exploration) 72 (2019): 122–38. http://dx.doi.org/10.3124/segj.72.122.

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42

Oshida, Atsushi, Toi Tachibana, Tomonori Sumi, and Ryuji Kubota. "Development of a new ocean bottom gravimeter and its application to exploration of seafloor massive sulfide deposits." BUTSURI-TANSA(Geophysical Exploration) 73 (2020): 23–32. http://dx.doi.org/10.3124/segj.73.23.

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43

Ren, Mengyi, Jianping Chen, Ke Shao, and Sheng Zhang. "Metallogenic information extraction and quantitative prediction process of seafloor massive sulfide resources in the Southwest Indian Ocean." Ore Geology Reviews 76 (July 2016): 108–21. http://dx.doi.org/10.1016/j.oregeorev.2016.01.008.

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44

Juliani, Cyril, and Steinar Løve Ellefmo. "Probabilistic estimates of permissive areas for undiscovered seafloor massive sulfide deposits on an Arctic Mid-Ocean Ridge." Ore Geology Reviews 95 (April 2018): 917–30. http://dx.doi.org/10.1016/j.oregeorev.2018.04.003.

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45

Schardt, C., J. Yang, and R. Large. "Formation of massive sulfide ore deposits on the seafloor —constraints from numerical heat and fluid flow modeling." Journal of Geochemical Exploration 78-79 (May 2003): 257–59. http://dx.doi.org/10.1016/s0375-6742(03)00040-2.

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46

Marques, Ana Filipa A., Fernando J. A. S. Barriga, and Steven D. Scott. "Sulfide mineralization in an ultramafic-rock hosted seafloor hydrothermal system: From serpentinization to the formation of Cu–Zn–(Co)-rich massive sulfides." Marine Geology 245, no. 1-4 (2007): 20–39. http://dx.doi.org/10.1016/j.margeo.2007.05.007.

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47

Yergeau, D., P. Mercier-Langevin, B. Dubé, et al. "The Westwood Deposit, Southern Abitibi Greenstone Belt, Canada: An Archean Au-Rich Polymetallic Magmatic-Hydrothermal System—Part II. Hydrothermal Alteration, Mineralization, and Geologic Model." Economic Geology 117, no. 3 (2022): 577–608. http://dx.doi.org/10.5382/econgeo.4879.

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Abstract The Westwood deposit, located in the Archean Doyon-Bousquet-LaRonde mining camp in the southern Archean Abitibi greenstone belt, contains 4.5 Moz (140 metric t) of gold. The deposit is hosted in the 2699–2695 Ma submarine, tholeiitic to calc-alkaline volcanic, volcaniclastic, and intrusive rocks of the Bousquet Formation. The deposit is located near the synvolcanic (ca. 2699–2696 Ma) Mooshla Intrusive Complex that hosts the Doyon epizonal intrusion-related Au ± Cu deposit, whereas several Au-rich volcanogenic massive sulfide (VMS) deposits are present east of the Westwood deposit. The

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48

Voudouris, Panagiotis, Marianna Kati, Andreas Magganas, et al. "Arsenian Pyrite and Cinnabar from Active Submarine Nearshore Vents, Paleochori Bay, Milos Island, Greece." Minerals 11, no. 1 (2020): 14. http://dx.doi.org/10.3390/min11010014.

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Active, shallow-water (2–10 m below sea level) and low temperature (up to 115 °C) hydrothermal venting at Paleochori Bay, nearshore Milos Island, Greece, discharges CO2 and H2S rich vapors (e.g., low-Cl fluid) and high-salinity liquids, which leads to a diverse assemblage of sulfide and alteration phases in an area of approximately 1 km2. Volcaniclastic detritus recovered from the seafloor is cemented by hydrothermal pyrite and marcasite, while semi-massive to massive pyrite-marcasite constitute mounds and chimney-like edifices. Paragenetic relationships indicate deposition of two distinct min

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Kitada, Kazuya, Yoshinori Sanada, Yasuhiro Yamada, et al. "Exploration of Seafloor Massive Sulfide deposits using natural gamma-ray logging: An application of through-the-bit logging." BUTSURI-TANSA(Geophysical Exploration) 73 (2020): 33–41. http://dx.doi.org/10.3124/segj.73.33.

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Monecke, T., S. Petersen, and M. D. Hannington. "Constraints on Water Depth of Massive Sulfide Formation: Evidence from Modern Seafloor Hydrothermal Systems in Arc-Related Settings." Economic Geology 109, no. 8 (2014): 2079–101. http://dx.doi.org/10.2113/econgeo.109.8.2079.

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