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Relevant bibliographies by topics / Seafloor massive sulfide

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Journal articles

Academic literature on the topic 'Seafloor massive sulfide'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 January 2023

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Journal articles on the topic "Seafloor massive sulfide"

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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