Works matching IS 00264598 AND DT 2023 AND VI 58 AND IP 5
Results: 9
Sulfide anatexis during high-grade metamorphism: a case study from the Bodenmais SEDEX deposit, Germany.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 987, doi. 10.1007/s00126-023-01166-y
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Textural and geochemical evidence for two-stage mineralisation at the Kamoa-Kakula Cu deposits, Central African Copperbelt.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 825, doi. 10.1007/s00126-023-01165-z
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Recognition of a ca. 130 Ma Makeng-Yangshan iron skarn belt in the Southeastern China: evidence from garnet in situ U–Pb geochronology.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 925, doi. 10.1007/s00126-023-01164-0
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Textural and compositional constraints on the origin, thermal history, and REE mobility in the Lakeh Siah iron oxide-apatite deposit—NE Bafq, Iran.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 963, doi. 10.1007/s00126-023-01163-1
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Thermal history of Carlin-type gold deposits in Yukon (Canada) as revealed by organic matter geothermometry, clumped isotope data, fluid inclusion microthermometry, and apatite fission-track analyses.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 903, doi. 10.1007/s00126-023-01162-2
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Insights into the metamorphic history and origin of flake graphite mineralization at the Graphite Creek graphite deposit, Seward Peninsula, Alaska, USA.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 939, doi. 10.1007/s00126-023-01161-3
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Petrogenesis of thick, high-grade PGE mineralisation in the Flatreef, northern Bushveld Complex.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 881, doi. 10.1007/s00126-022-01156-6
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Feedbacks between fast brittle faulting, hydrothermal fluid flow, and metal transport within carbonated ultramafics (Ligurian Western Alps, Italy).
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 833, doi. 10.1007/s00126-022-01142-y
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Germanium- and gallium-rich sphalerite in Mississippi Valley–type deposits: the San Vicente district and the Shalipayco deposit, Peru.
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- Mineralium Deposita, 2023, v. 58, n. 5, p. 853, doi. 10.1007/s00126-023-01160-4
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