1993
DOI: 10.1016/0169-1368(93)90027-v
|View full text |Cite
|
Sign up to set email alerts
|

Remobilization, syn-tectonic processes and massive sulphide deposits

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

2
29
0

Year Published

1994
1994
2015
2015

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 83 publications
(33 citation statements)
references
References 56 publications
2
29
0
Order By: Relevance
“…'Chalcopyrite disease' (Wiggins and Craig, 1980;Barton and Bethke, 1987) is generally present in sphalerite. (b) Brittle behaviour is displayed by pyrite and arsenopyrite that constitute the high strength minerals in the deposits (Graf and Skinner, 1970;Clark and Kelly, 1976;Pedersen, 1980;Marshall and Gilligan, 1993). The small pyrite and arsenopyrite grains are anhedral or subhedral crystals while the coarser grains are typically subhedral to euhedral (Fig.…”
Section: Deformation Structures and Texturesmentioning
confidence: 97%
“…'Chalcopyrite disease' (Wiggins and Craig, 1980;Barton and Bethke, 1987) is generally present in sphalerite. (b) Brittle behaviour is displayed by pyrite and arsenopyrite that constitute the high strength minerals in the deposits (Graf and Skinner, 1970;Clark and Kelly, 1976;Pedersen, 1980;Marshall and Gilligan, 1993). The small pyrite and arsenopyrite grains are anhedral or subhedral crystals while the coarser grains are typically subhedral to euhedral (Fig.…”
Section: Deformation Structures and Texturesmentioning
confidence: 97%
“…Marshall and Gilligan (1993) have discussed several guidelines, the application of which ''require a thorough geometric and kinematic analysis on all scales," and the task is a difficult one. Both are capable of yielding the same or similar geometric relationships, fluid inclusion data, fluid chemistry, and metal and sulfur sources.…”
Section: Metamorphic Remobilizationmentioning
confidence: 99%
“…The extraction of base metals, especially Pb, from deeper crustal levels has been previously suggested and is supported by fluid inclusion data and isotope signatures (Beaudoin et al 1992ab;Costagliola et al 1999). The recognised high solubility of Pb and Zn at high temperatures (e.g., Helgeson 1969;Hemley et al 1992) provides the thermodynamic base for models in which metamorphosed base metal deposits lose Pb and Zn to the metamorphic fluids that then potentially deposit these metals into late-metamorphic structures (Marshall and Gilligan 1993;Tomkins et al 2007). Nevertheless, it has proven difficult to quantify the amounts of dissolution of base metals in these and similar source region environments.…”
Section: Introductionmentioning
confidence: 81%