Coupled zircon-rutile U-Pb chronology : LA ICP-MS dating, geological significance and applications to Sediment Provenance in the Eastern Himalayan-Indo-Burman Region

dc.contributor.authorBracciali, Lauraen_ZA
dc.date.accessioned2019-11-13T07:25:16Z
dc.date.available2019-11-13T07:25:16Z
dc.date.issued2019-11-05
dc.descriptionCITATION: Bracciali, L. 2018. Coupled zircon-rutile U-Pb chronology : LA ICP-MS dating, geological significance and applications to Sediment Provenance in the Eastern Himalayan-Indo-Burman Region. Geosciences, 9(11):467, doi:10.3390/geosciences9110467.en_ZA
dc.descriptionThe original publication is available at http://www.mdpi.comen_ZA
dc.descriptionPublication of this article was funded by the Stellenbosch University Open Access Fund.en_ZA
dc.description.abstractU-Pb dating by LA ICP-MS is one of the most popular and successful isotopic techniques available to the Earth Sciences to constrain timing and rates of geological processes thanks to its high spatial resolution, good precision (absolute U/Pb age resolution of ca. 2%, 2s), rapidity and relative affordability. The significant and continuous improvement of instrumentation and approaches has opened new fields of applications by extending the range of minerals that can be dated by this method. Following the development and distribution to the community of good quality reference materials in the last decade, rutile U-Pb thermochronology (with a precision only slightly worse than zircon) has become a commonly used method to track cooling of deep-seated rocks. Its sensitivity to mid- to low-crustal temperatures (~450 °C to 650 °C) is ideal to constrain exhumation in active and ancient orogens as well as thermal evolution of slow-cooled terranes. Recrystallization and secondary growth during metamorphism and the presence of grain boundary fluids can also affect the U-Pb isotopic system in rutile. A growing body of research focusing on U-Pb dating of rutile by LA ICP-MS is greatly improving our understanding of the behavior of this mineral with regards to retention of radiogenic Pb. This is key to fully exploit its potential as a tracker of geological processes. The latest developments in this field are reviewed in this contribution. The combined application of U-Pb zircon and rutile chronology in provenance studies, particularly when complemented by lower-T thermochronometry data, allows the isotopic characterization of the sources across a wide range of temperatures. The benefits of applying detrital zircon-rutile U-Pb chronology as a coupled provenance proxy are presented here, with a focus on the Eastern Himalayan-Indo-Burman region, where a growing number of successful studies employs such an approach to help constrain river drainage and basin evolution and to infer feedback relationships between erosion, tectonics and climate.en_ZA
dc.description.urihttps://www.mdpi.com/2076-3263/9/11/467
dc.description.versionPublisher's versionen_ZA
dc.format.extent29 pages : illustrations, mapsen_ZA
dc.identifier.citationBracciali, L. 2018. Coupled zircon-rutile U-Pb chronology : LA ICP-MS dating, geological significance and applications to Sediment Provenance in the Eastern Himalayan-Indo-Burman Region. Geosciences, 9(11):467, doi:10.3390/geosciences9110467en_ZA
dc.identifier.issn2077-1444 (online)
dc.identifier.otherdoi:10.3390/geosciences9110467
dc.identifier.urihttp://hdl.handle.net/10019.1/106834
dc.language.isoen_ZAen_ZA
dc.publisherMDPIen_ZA
dc.rights.holderAuthors retain copyrighten_ZA
dc.subjectRutile -- Eastern Himlayan-Indo-Burman Regionen_ZA
dc.subjectU-Pb thermochronologyen_ZA
dc.subjectRutile U-Pb thermochronologyen_ZA
dc.subjectSediment provenanceen_ZA
dc.titleCoupled zircon-rutile U-Pb chronology : LA ICP-MS dating, geological significance and applications to Sediment Provenance in the Eastern Himalayan-Indo-Burman Regionen_ZA
dc.typeArticleen_ZA
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