| nr |
titel |
auteur |
tijdschrift |
jaar |
jaarg. |
afl. |
pagina('s) |
type |
| 1 |
Barite–silica mineralization at the inter-Ordovician unconformity in southwestern Sardinia (Italy): a fluid inclusion study
|
Fedele, L.
|
|
2002
|
77 |
3-4 |
p. 197-213
|
artikel
|
| 2 |
Corundum-bearing amphibolites from the metamorphic basement of the Krivaja–Konjuh ultramafic massif (Dinaride Ophiolite Zone, Bosnia)
|
Operta, M.
|
|
2002
|
77 |
3-4 |
p. 287-295
|
artikel
|
| 3 |
Garnets in volcanic breccias of the Phlegraean Fields (southern Italy): mineralogical, geochemical and genetic features
|
Naimo, D.
|
|
2002
|
77 |
3-4 |
p. 259-270
|
artikel
|
| 4 |
Magnetite, ilmenite and ulvite in rocks and ore deposits: petrography, microprobe analyses and genetic implications
|
Mücke, A.
|
|
2002
|
77 |
3-4 |
p. 215-234
|
artikel
|
| 5 |
Microtextures and crystal chemistry in P21/c pigeonites
|
Tribaudino, M.
|
|
2002
|
77 |
3-4 |
p. 161-176
|
artikel
|
| 6 |
Reply to comment: “The Nakhla Martian meteorite is a cumulate igneous rock” by A. Treiman
|
Varela, M. E.
|
|
2002
|
77 |
3-4 |
p. 279-285
|
artikel
|
| 7 |
The Nakhla Martian meteorite is a cumulate igneous rock. Comment on “Glass-bearing inclusions in Nakhla (SNC meteorite) augite: heterogeneously trapped phases” (2001) by M. E. Varela, G. Kurat, and R. Clocchiatti
|
Treiman, A. H.
|
|
2002
|
77 |
3-4 |
p. 271-277
|
artikel
|
| 8 |
The petrogenetic association of carbonatite and alkaline magmatism: constraints from the Masfut-Rawda Ridge, Northern Oman Mountains
|
Nasir, S.
|
|
2002
|
77 |
3-4 |
p. 235-258
|
artikel
|
| 9 |
Washing soda (natron), Na2CO3·10H2O, revised: crystal structures at low and ambient temperatures
|
Libowitzky, E.
|
|
2002
|
77 |
3-4 |
p. 177-195
|
artikel
|
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