Evidence of a close link between petrology and isotope records: Constraints from SEM, EMP, TEM and is situ 40Ar-39Ar laser analyses on multiple generations of white micas (Lanterman Range, Antarctica)

Earth and Planetary Science Letters

Volumn 192, Issue 3, 2001, Pages 389-405

  Di Vincenzo, Gianfranco ^a   Ghiribelli, Barbara ^b   Giorgetti, Giovanna ^b   Palmeri, Rosaria ^b  

^a CNR   (Italy)

^b UNIVERSITY OF SIENA   (Italy)

Author keywords

Absolute age; Antarctica; Ar 40 Ar 39; Eclogite; In situ; Mica group

Indexed keywords

ARGON-ARGON DATING; ELECTRON MICROSCOPY; ISOTOPIC ANALYSIS; METAMORPHISM; MICA; PALEOZOIC; PETROGRAPHY;

ANTARCTICA;

EID: 0035170181     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00454-X     Document Type: Article

References (39)

1. Closure temperature in cooling geochronological and petrological systems
2. 39Ar and microprobe analyses on white micas
3. * from muscovite during polymetamorphism
4. On the thermal stability of Rb Sr and K-Ar biotite systems: Evidence from coexisting Sveconorwegian (ca 870 Ma) and Caledonian (ca 400 Ma) biotites in SW Norway
5. Retention of Precambrian Rb/Sr phlogopite ages through Caledonian eclogite facies metamorphism. Berger Arc Complex, W-Norway
6. Isotopic closure
7. The pre Beacon geology of northern Victoria Land: A review
8. Metamorphic facies of the Ross orogeny in the southern Wilson Terrane of northern Victoria Land, Antarctica
9. Contrasting metamorphic belts in north Victoria Land, Antarctica
10. Eclogite at the Antarctic palaeo-Pacific margin of Gondwana (Lanterman Range, northern Victoria Land, Antarctica)
11. The northern Victoria Land segment of the Antarctic paleo-Pacific margin of Eastern Gondwana: New constraints from the Lanterman and Mountaineer Ranges
12. Metamorphism and structural relations of the Lanterman metamorphics, North Victoria Land Antarctica
13. Petrology and geochronology of eclogites from the Lanterman Range Antarctica
14. 39Ar investigation of high-pressure metamorphism and the retrogressive history of mafic eclogites from the Lanterman Range (Antarctica): Evidence against a simple temperature control on argon transport in amphibole
15. 39Ar ages
16. Geological Mapping and field relationships of eclogites from the Lanterman Range (northern Victoria Land, Antarctica)
17. The diagenetic to low-grade metamorphic evolution of matrix white micas in the system muscovite-paragonite in a mud-rock from central Wales, United Kingdom
18. 39Ar dating standard, MMhb-1
19. Symbols for rock-forming minerals
20. Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz
21. 2O
22. High-pressure relics in metasediments intercalated with the Weissenstein eclogite, Munchberg gneiss complex, Bavaria
23. Cation-diffusion-induced characteristic beam damage in transmission electron microscope images of micas
24. Eocene age of eclogite metamorphism in Pakistan Himalaya: Implication for India Eurasia collision
25. 39Ar technique
26. 39Ar UV-laser ablation analysis
27. 39Ar laserprobe ages of metamorphic micas and amphibole of the Wilson Terrane and Dessent Unit, Northern Victoria Land (Antarctica): Their bearing on the regional post-metamorphic cooling history
28. Constraining the timing of the structural evolution along terrane boundaries: The case of the Lanterman Fault Zone, northern Victoria Land, Antarctica, EUGXI
29. Multipath diffusion in geochronology
30. 39Ar dating of high pressure metamorphic micas from the Gran Paradiso area (western Alps): Evidence against the blocking temperature concept
31. 40Ar dating of multiply zoned amphibole generation (Malenco, Italy)
32. 39Ar step heating and single grain laser probe dating
33. Determinations of high spatial resolution argon isotope variations in metamorphic biotites
34. Limited mobility of argon in a metamorphic terrane
35. The Qinglonshan oxygen and hydrogen isotope anomaly near Donghai in Jiangsu Province, China
36. Synchroton powder diffraction study of pheogite 3T from the Dora-Maira massif: P V-T equation of state and petrological consequences