Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4727860 | Gondwana Research | 2009 | 10 Pages |
Abstract
Geodynamic processes, like amalgamation and continental dispersal, control the thermobarometric history of the Earth's crust. Due to its central position, Madagascar is the ideal location for studying important aspects of the amalgamation and breakup of the Gondwana supercontinent. Using geochronological methods (e. g. U-Pb zircon and monazite as well as titanite and apatite fission-track dating), a detailed cooling path for the Bemarivo Belt of northern Madagascar has been deciphered. New SHRIMP zircon ages of ca. 540Â Ma and published monazite ages of ca. 515Â Ma allow to estimate the duration of the high/ultrahigh-temperature metamorphism related to the early Palaeozoic continental collision during Gondwana formation. The breakup of this supercontinent was associated with crustal thinning, brittle deformation and denudation along the evolving sedimentary basins recorded by the titanite and apatite fission-track ages ranging between ca. 320Â Ma and 160Â Ma.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Niels Jöns, Benjamin Emmel, Volker Schenk, Théodore Razakamanana,