Apatite and titanite from the Karrat Group, Greenland; implications for charting the thermal evolution of crust from the U-Pb geochronology of common Pb bearing phases

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Apatite and titanite from the Karrat Group, Greenland; implications for charting the thermal evolution of crust from the U-Pb geochronology of common Pb bearing phases

Titanite and apatite have Pb closure temperatures of ~700 °C and 450–550 °C, respectively, allowing different points on a cooling trajectory to be determined. However, both phases typically accommodate moderate to significant quantities of common Pb. Understanding the thermal diffusivity of a specif...

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Bibliographic Details
Main Authors:	Kirkland, Chris, Hollis, Julie, Danisik, Martin, Petersen, J., Evans, Noreen, McDonald, B.
Format:	Journal Article
Published:	Elsevier BV 2017
Online Access:	http://hdl.handle.net/20.500.11937/56772

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