| nr |
titel |
auteur |
tijdschrift |
jaar |
jaarg. |
afl. |
pagina('s) |
type |
| 1 |
A comparison of the lead phosphates from the Oxidised Zone, broken hill ore body, with those of some other Australian localities
|
Barclay, C. J.
|
|
1971
|
18 |
3 |
p. 207-213
|
artikel
|
| 2 |
Cainozoic Stratigraphy of the lake Eyre basin and part of the arid region lying to the South
|
Jessup, R. W.
|
|
1971
|
18 |
3 |
p. 303-331
|
artikel
|
| 3 |
Calcite precipitation and Recrystallization fabrics—their significance in Jurassic Limestones of Europe
|
Davies, Peter J.
|
|
1971
|
18 |
3 |
p. 279-292
|
artikel
|
| 4 |
Corrigenda
|
|
|
1971
|
18 |
3 |
p. 332
|
artikel
|
| 5 |
Editorial board
|
|
|
1971
|
18 |
3 |
p. 1
|
artikel
|
| 6 |
Geological interpretation of the Cootamundra gravity high, New South Wales
|
Watts, M. D.
|
|
1971
|
18 |
3 |
p. 229-234
|
artikel
|
| 7 |
Kaolinite Claystones associated with the Wongawilli seam in the southern part of the Sydney basin
|
Loughnan, F. C.
|
|
1971
|
18 |
3 |
p. 293-302
|
artikel
|
| 8 |
Occurrence and significance of Ischadites Murchison in Ordovician Limestones at Bowan Park, New South Wales
|
Semeniuk, Vic
|
|
1971
|
18 |
3 |
p. 235-241
|
artikel
|
| 9 |
Retrograde Schists of the Amphibolite Facies at broken hill, New South Wales
|
Vernon, R. H.
|
|
1971
|
18 |
3 |
p. 267-277
|
artikel
|
| 10 |
Rubidium-strontium geochronology of the encounter bay granite and adjacent Metasedimentary rocks, South Australia
|
Dasch, E. J.
|
|
1971
|
18 |
3 |
p. 259-266
|
artikel
|
| 11 |
Structural analysis of Bermagui area, N.S.W.
|
Williams, Paul F.
|
|
1971
|
18 |
3 |
p. 215-228
|
artikel
|
| 12 |
The gravitational field and the Geoid of Australia
|
Grushinsky, N. P.
|
|
1971
|
18 |
3 |
p. 183-199
|
artikel
|
| 13 |
The mineralogy of the Gosse pile ultramafic intrusion, central Australia. II. Pyroxenes
|
Moore, A. C.
|
|
1971
|
18 |
3 |
p. 243-258
|
artikel
|
| 14 |
The South Australian earthquake of January 7, 1971 and aftershocks
|
Stewart, I. C. F.
|
|
1971
|
18 |
3 |
p. 201-205
|
artikel
|
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