Authigenetic K-feldspars and their relations to Sn polymetallic mineralization in the Dachang ore field
Sn-polymetallic ores at Dachang, Guangxi Autonomous Region, China, are hosted in Middle-Upper Devonian reef limestones, siliceous rocks, banded and lenticular limestones, etc. Two types of orebodies can be distinguished according to their relations to the bedding: one is distributed along the beddin...
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| Hauptverfasser: | , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
1993
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| In: |
Chinese journal of geochemistry
Year: 1993, Jahrgang: 12, Heft: 3, Pages: 270-288 |
| ISSN: | 1993-0364 |
| DOI: | 10.1007/BF02843366 |
| Online-Zugang: | Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1007/BF02843366
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| Verfasserangaben: | Pan Jiahua, G.C. Amstutz |
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| 520 | |a Sn-polymetallic ores at Dachang, Guangxi Autonomous Region, China, are hosted in Middle-Upper Devonian reef limestones, siliceous rocks, banded and lenticular limestones, etc. Two types of orebodies can be distinguished according to their relations to the bedding: one is distributed along the bedding and the other cuts across the bedding. Sn and sulfide orebodies associated with K-feldspars are mostly characterized by laminated ore structure. | ||
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| 650 | 4 | |a Dachang Sn deposit | |
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