Australian Journal of Earth Sciences


ISSN: 0812-0099        年代:1991
当前卷期:Volume 38  issue 5     [ 查看所有卷期 ]

年代:1991
 
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     Volume 38  issue 5
1. Geological relationships in high‐grade gneiss of the Brattstrand Bluffs coastline, Prydz Bay, East Antarctica
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  497-519

I. C. W. Fitzsimons,   S. L. Harley,  

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2. Introduction
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  523-524

DavidJ. Whitford,   PeterK. Kinny,  

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3. Physical and chemical evidence on the cause and source characteristics of flood basalt volcanism
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  525-544

R. W. Carlson,  

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4. A comparison of Sr‐Nd‐Pb isotopes in young and old continental lithospheric mantle: Patagonia and Eastern China
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  545-557

R.E. Zartman,   K. Futa,   Z.C. Peng,  

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5. Evolution of the lithosphere and its interaction with the underlying mantle as inferred from noble gas isotopes
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  559-567

I. Kaneoka,   N. Takaoka,  

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6. Re‐Os isotopic constraints on the formation of mantle and crustal reservoirs
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  569-576

C.E. Martin,   B.K. Esser,   K.K. Turekian,  

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7. Destructive margin magmatism and the contributions from the mantle wedge and subducted crust
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  577-594

C.J. Hawkesworth,   J.M. Hergt,   F. McDermott,   R.M. Ellam,  

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8. The Canadian Cordillera as a modern analogue of Proterozoic crustal growth
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  595-611

S. D. Samson,   P. J. Patchett,  

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9. The persistent myth of crustal growth
  Australian Journal of Earth Sciences,   Volume  38,   Issue  5,   1991,   Page  613-630

R. L. Armstrong,  

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