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Strengthening the link between geochronology, textures and petrology

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dc.contributor.authorMueller, Wolfgang
dc.date.accessioned2015-12-13T22:34:59Z
dc.date.available2015-12-13T22:34:59Z
dc.date.issued2003
dc.date.updated2015-12-11T09:25:12Z
dc.description.abstractTime must be integrated with other geologic parameters such as pressure-temperature (P-T), composition or structural-textural information in order to quantify the dynamics of geologic processes like mountain building, faulting, metamorphism or magmatism.
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/76379
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: dating method; deformation; geochronology; P-T-t path; petrology; structural geology; texture Ar-40/Ar-39; Dates; Deformation; Duration; Fault zones; Garnet; Geochronology; Laser ablation; Lu-Hf; Mylonites; P-T-t paths; Petrology; Rates; Rb/Sr; Sm/Nd; Structural geology; Textures; U-Th-Pb
dc.titleStrengthening the link between geochronology, textures and petrology
dc.typeJournal article
local.bibliographicCitation.lastpage251
local.bibliographicCitation.startpage237
local.contributor.affiliationMueller, Wolfgang, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidMueller, Wolfgang, u4097174
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040303 - Geochronology
local.identifier.absfor040312 - Structural Geology
local.identifier.ariespublicationMigratedxPub5193
local.identifier.citationvolume206
local.identifier.doi10.1016/S0012-821X(02)01007-5
local.identifier.scopusID2-s2.0-0037441659
local.type.statusPublished Version

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