Geochemical Characteristics of Mineral Assemblages from the Yamansu Iron Deposit, NW China, and Their Metallogenic Implications Article Swipe
Zhiyuan Sun
,
Jingbin Wang
,
Yuwang Wang
,
Lingli Long
·
YOU?
·
· 2019
· Open Access
·
· DOI: https://doi.org/10.3390/min10010039
YOU?
·
· 2019
· Open Access
·
· DOI: https://doi.org/10.3390/min10010039
The Yamansu deposit, which is hosted in the volcanic-sedimentary sequence of the Carboniferous Yamansu Formation in Eastern Tianshan, NW China, contains many skarns, and the orebodies occur in the ore district in stratoidal, banded or lenticular forms. Four alteration stages, namely, albite–tourmaline–apatite–Grt1 (Stage I), K-feldspar–Grt2 (Stage II), magnetite–chlorite–epidote (Stage III), and quartz–calcite–axinite–Grt3 (Stage IV), are distinguished in the Yamansu deposit. The mineral geochemistry associated with each different stage is presented to provide a better understanding of the corresponding metallogenic processes. The ore-forming fluid in Stage I was derived from a magmatic–hydrothermal source and formed at high temperatures with many volatiles. This ore-forming fluid, which contained considerable metallogenic materials during the early stage, likely experienced diffusive metasomatism in a closed system with low water/rock (W/R) ratios. Mineral geochemical analyses show that the Fe content gradually increases from Stage I to Stage II, indicating that accumulated ore-forming materials were available during changes in the physicochemical conditions from a reducing environment with neutral pH to oxidizing conditions with mildly acidic pH. During the main metallogenic stage (Stage III), mineral assemblages reflect moderate- to high-temperature conditions, and the ore-forming fluid was created and destroyed periodically; the magnetite ores were deposited in a fluctuating fluid system. The multilayered orebodies, multigenerational garnets, and minerals with oscillatory zoning indicate that the ore-forming fluid may have developed periodic fluctuations, and this special multistage fluctuation of the hydrothermal fluid in the Yamansu deposit was the key factor controlling the multiple extraction, enrichment and precipitation of metallogenic materials.
Related Topics
Concepts
Geology
Geochemistry
Skarn
Hydrothermal circulation
Epidote
Mineral
Metasomatism
Albite
Stage (stratigraphy)
Magnetite
Magmatic water
Quartz
Feldspar
Fluid inclusions
Ore genesis
Sedimentary rock
Mineralogy
Chlorite
Chemistry
Organic chemistry
Seismology
Mantle (geology)
Paleontology
Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.3390/min10010039
- https://www.mdpi.com/2075-163X/10/1/39/pdf?version=1577774250
- OA Status
- gold
- Cited By
- 5
- References
- 64
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W2997000225
All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W2997000225Canonical identifier for this work in OpenAlex
- DOI
-
https://doi.org/10.3390/min10010039Digital Object Identifier
- Title
-
Geochemical Characteristics of Mineral Assemblages from the Yamansu Iron Deposit, NW China, and Their Metallogenic ImplicationsWork title
- Type
-
articleOpenAlex work type
- Language
-
enPrimary language
- Publication year
-
2019Year of publication
- Publication date
-
2019-12-31Full publication date if available
- Authors
-
Zhiyuan Sun, Jingbin Wang, Yuwang Wang, Lingli LongList of authors in order
- Landing page
-
https://doi.org/10.3390/min10010039Publisher landing page
- PDF URL
-
https://www.mdpi.com/2075-163X/10/1/39/pdf?version=1577774250Direct link to full text PDF
- Open access
-
YesWhether a free full text is available
- OA status
-
goldOpen access status per OpenAlex
- OA URL
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https://www.mdpi.com/2075-163X/10/1/39/pdf?version=1577774250Direct OA link when available
- Concepts
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Geology, Geochemistry, Skarn, Hydrothermal circulation, Epidote, Mineral, Metasomatism, Albite, Stage (stratigraphy), Magnetite, Magmatic water, Quartz, Feldspar, Fluid inclusions, Ore genesis, Sedimentary rock, Mineralogy, Chlorite, Chemistry, Organic chemistry, Seismology, Mantle (geology), PaleontologyTop concepts (fields/topics) attached by OpenAlex
- Cited by
-
5Total citation count in OpenAlex
- Citations by year (recent)
-
2023: 1, 2022: 2, 2020: 2Per-year citation counts (last 5 years)
- References (count)
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64Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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