Mineralisation from Vall de Ribes area (Eastern Pyrenees, Spain)

C. Ayora; E. Cardellach; R. Phillips

doi:10.1007/BF00202734

Mineralisation from Vall de Ribes area (Eastern Pyrenees, Spain)

C. Ayora, E. Cardellach, R. Phillips

Department of Geology

Research output: Contribution to journal › Article › Research › peer-review

3 Citations (Scopus)

Abstract

Vein mineralisation with no preferred orientation, cutting lower Palaeozoic rocks, and local replacement deposits in dolomite show a zoning in tungsten-bismuth, arsenic and antimony minerals away from the adjacent late-Hercynian Costabona granite. A local reversed zoning is related to higher temperatures indicated by fluid inclusion study. Many of the minerals have not previously been reported from this area. © 1981 Springer-Verlag.

Original language	English
Pages (from-to)	195-204
Journal	Mineralium Deposita
Volume	16
Issue number	2
DOIs	https://doi.org/10.1007/BF00202734
Publication status	Published - 1 Aug 1981

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title = "Mineralisation from Vall de Ribes area (Eastern Pyrenees, Spain)",

abstract = "Vein mineralisation with no preferred orientation, cutting lower Palaeozoic rocks, and local replacement deposits in dolomite show a zoning in tungsten-bismuth, arsenic and antimony minerals away from the adjacent late-Hercynian Costabona granite. A local reversed zoning is related to higher temperatures indicated by fluid inclusion study. Many of the minerals have not previously been reported from this area. {\textcopyright} 1981 Springer-Verlag.",

author = "C. Ayora and E. Cardellach and R. Phillips",

year = "1981",

month = aug,

day = "1",

doi = "10.1007/BF00202734",

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journal = "Mineralium Deposita",

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T1 - Mineralisation from Vall de Ribes area (Eastern Pyrenees, Spain)

AU - Ayora, C.

AU - Cardellach, E.

AU - Phillips, R.

PY - 1981/8/1

Y1 - 1981/8/1

N2 - Vein mineralisation with no preferred orientation, cutting lower Palaeozoic rocks, and local replacement deposits in dolomite show a zoning in tungsten-bismuth, arsenic and antimony minerals away from the adjacent late-Hercynian Costabona granite. A local reversed zoning is related to higher temperatures indicated by fluid inclusion study. Many of the minerals have not previously been reported from this area. © 1981 Springer-Verlag.

AB - Vein mineralisation with no preferred orientation, cutting lower Palaeozoic rocks, and local replacement deposits in dolomite show a zoning in tungsten-bismuth, arsenic and antimony minerals away from the adjacent late-Hercynian Costabona granite. A local reversed zoning is related to higher temperatures indicated by fluid inclusion study. Many of the minerals have not previously been reported from this area. © 1981 Springer-Verlag.

U2 - 10.1007/BF00202734

DO - 10.1007/BF00202734

M3 - Article

VL - 16

SP - 195

EP - 204

JO - Mineralium Deposita

JF - Mineralium Deposita

SN - 0026-4598

IS - 2

ER -