Sinking intrusion model for the emplacement of garnet-bearing peridotites into continent collision orogens: Reply

Geology

Volumn 27, Issue 5, 1999, Pages 477-478

  Brueckner, Hannes K ^a,b  

^a CITY UNIVERSITY OF NEW YORK   (United States)

^b Lamont Doherty Earth Observatory of Columbia University   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ARC-CONTINENT COLLISION; EMPLACEMENT; GARNET; IGNEOUS INTRUSION; PERIDOTITE;

EID: 80053483598     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/0091-7613(1999)027<0477:SIMFTE>2.3.CO;2     Document Type: Letter

References (5)

1. Brueckner,H. K., 1998, Sinking intrusion model for the emplacement of garnet-bearing peridotites into continent collision orogens: Geology, v. 26, p. 631-634.
2. Brueckner, H. K., and Medaris, L. G., Jr., 1998a, A tale of two orogens: The contrasting TPt history and geochemical evolution of mantle in high- and ultrahighpressure metamorphic terranes of the Norwegian Caledonides and the Czech Variscides: Schweizerische Mineralogische und Petrographische Mitteilungen, v. 78, p. 293-307.
3. Brueckner, H. K., and Medaris, L. G., Jr., 1998b, A general model for the intrusion and evolution of peridotites in high-pressure and ultrahigh-pressure metamorphic terranes: International Workshop on UHP Metamorphism and Exhumation, p. A-1-5.
4. Smith, D. C., 1995, Microcoesites and microdiamonds in Norway: An overview, in Coleman, R. G., and Wang, X., eds., Ultrahigh pressure metamorphism: Cambridge, UK, Cambridge University Press, p. 299-355.
5. Terry, M. P., and Robinson, P., 1998, Eclogite-facies structural features and their bearing on mechanisms for production and exhumation of high-pressure rocks, Western Gneiss region, Norway, including the microdiamond-bearing gneiss at Fjørtoft: International Workshop on UHP Metamorphism and Exhumation, p. A-74-78.