Watch the Dallas Symposium LIVE, and fundraiser auction
Ticket proceeds support mindat.org! - click here...
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Hoffman, P. F. (2006) Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22300.1

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleEvidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: COMMENT
JournalGeology
AuthorsHoffman, P. F.Author
Year2006 (January 1)Volume34
Issue1
PublisherGeological Society of America
DOIdoi:10.1130/g22300.1Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID139623Long-form Identifiermindat:1:5:139623:6
GUID0
Full ReferenceHoffman, P. F. (2006) Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22300.1
Plain TextHoffman, P. F. (2006) Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22300.1
In(2006, January) Geology Vol. 34 (1) Geological Society of America

See Also

These are possibly similar items as determined by title/reference text matching only.

Stern, R. J. (2006) Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: REPLY. Geology, 34 (1) doi:10.1130/g23026.1
Stern, Robert J. (2005) Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time. Geology, 33 (7) 557 doi:10.1130/g21365.1
Clift, P. D., Ruiz, G. M. H. (2007) How does the Nazca Ridge subduction influence the modern Amazonian foreland basin?: COMMENT and REPLY: COMMENT. Geology, 35 (1) doi:10.1130/g24355c.1
Berner, R. A., Ward, P. D. (2006) Positive Reinforcement, H2S, and the Permo-Triassic Extinction: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22641.1
Schwartzman, D. (2006) Role of river-suspended material in the global carbon cycle: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22686c.1
Hermann, Joerg (2003) Carbon recycled into deep Earth: Evidence from dolomite dissociation in subduction-zone rocks: Comment and Reply. Geology, 31 (1) doi:10.1130/0091-7613-31.1.e4
Zhu, Yongfeng (2003) Carbon recycled into deep Earth: Evidence from dolomite dissociation in subduction-zone rocks: Comment and Reply. Geology, 31 (1) doi:10.1130/0091-7613-31.1.e5
Berlo, K., Turner, S., Blundy, J., Hawkesworth, C. (2006) 226Ra/230Th excess generated in the lower crust: Implications for magma transport and storage time scales: Comment and Reply: COMMENT. Geology, 34 (1) doi:10.1130/g22667.1
Platt, John, Houseman, Greg (2003) Evidence for active subduction beneath Gibraltar: Comment and Reply. Geology, 31 (1) doi:10.1130/0091-7613-31.1.e22
Dufek, J., Cooper, K. M. (2006) 226Ra/230Th excess generated in the lower crust: Implications for magma transport and storage time scales: Comment and Reply: REPLY. Geology, 34 (1) doi:10.1130/g23073.1
Ritz, J.-F. (2009) Extrusion tectonics and subduction in the eastern South Caspian region since 10 Ma: COMMENT. Geology, 37 (12) doi:10.1130/g25627c.1
 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are Β© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: August 18, 2025 08:38:52
Go to top of page