An isotopic mixing model for the origin of granitic rocks in southeastern Australia

Earth and Planetary Science Letters

Volumn 70, Issue 1, 1984, Pages 47-60

  Gray, C M ^a  

^a LA TROBE UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0021335857     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/0012-821X(84)90208-5     Document Type: Article

References (23)

1. Geology of the Berridale 1:100000 sheet 8625
2. Contrasts between I- and S-type granitoids of the Kosciusko Batholith
3. The Moruya Batholith and geochemical contrasts between the Moruya and Jindabyne suites
4. Granitoid types and their distribution in the Lachlan Fold Belt, southeastern Australia
5. Plutonic rocks of the Lachlan Mobile Zone
6. Sr-isotope evolution of granitoid source rocks
7. Nd isotopic characteristics of S- and I-type granites
8. Two contrasting granite types
9. Radiometric evidence for the age of emplacement and cooling of the Murrumbidgee Batholith
10. The age and origin of the Cooma Granite and its associated metamorphic zones, New South Wales
11. Petrological studies in the Ordovician of New South Wales, I. The Cooma Complex
12. The Cooma Granodiorite, Australia: an example of in situ crustal anatexis?
13. Ultrametamorphism and granitoid genesis
14. Petrogenetic mixing models and NdSr isotopic patterns
15. 86Sr ratios in oceanic basalts
16. 86Sr and trace element constraints on the petrogenesis of Aleutian island arc magmas
17. Petrogenesis of the Murrumbidgee Batholith ACT
18. 86Sr ratios in the Sierra Nevada Plutonic Province
19. Some petrological, geochemical and geochronological observations of the Peninsular Ranges Batholith near the international border of the U.S.A. and Mexico
20. Oxygen and strontium isotope relationships in the British late Caledonian granites
21. NdSr isotopic relationship in granitoid rocks and continental crustdevelopment: a chemical approach to orogenesis
22. A neodymium and strontium isotopic study of the Mesozoic calc-alkaline granitic batholiths of the Sierra Nevada and Peninsular Ranges, California
23. Strontium isotopic equilibration: a solution to a paradox