On the geodynamic setting of kimberlite genesis
Reference (40)
- et al.
Kimberlites: their relation to mantle hot spots, Earth Planet
Sci. Lett.
(1980) - et al.
Minimum continental velocities with respect to the pole since the Archaean
Tectonophysics
(1981) - et al.
Paleomagnetic poles and polarity zonation from Cambrian and Devonian strata of Arizona
Earth Planet. Sci. Lett.
(1977) - et al.
Apparent polar wander for the Atlantic-bordering continents: Late Carboniferous to Eocene
Earth Sci. Rev.
(1974) - et al.
Garnet peridotite xenoliths in Montana, U.S.A., kimberlite
Phys. Chem. Earth
(1975) Peridotite xenoliths and the dynamics of kimberlite intrusion
Kimberlites: strange bodies
EOS Trans. Am. Geophys. Union
(1981)Order-disorder kinetics of ferromagnesian silicates, and the cooling history of rocks
EOS Trans. Am. Geophys. Union
(1981)Kimberlites and Their Xenoliths
(1979)The kimberlites of the continental United States: a review
J. Geol.
(1976)
The kimberlites of the U.S.S.R.
Origin of kimberlite pipes by diapiric upwelling in the upper mantle
Nature
Chemical plumes in the mantle
Geol. Soc. Am. Bull.
Kimberlites and plate tectonics in Africa
Nature
An alternative hypothesis for the origin of west African kimberlites
Nature
Plate movement and continental magmatism
Nature
KAr and RbSr ages of some alkalic intrusives from central and eastern United States
Am. J. Sci.
Structural setting of kimberlites in southeastern Australia
Drift of major continental blocks since the Devonian
Nature
Paleopoles and paleolatitudes of North America, and speculations about displaced terrains
Can. J. Earth Sci.
Cited by (36)
Geodynamics of kimberlites on a cooling Earth: Clues to plate tectonic evolution and deep volatile cycles
2018, Earth and Planetary Science LettersCitation Excerpt :However, it is reasonable to conclude that enhanced rifting and drifting of tectonic plates with associated far-field stresses that propagate into cratonic continental interiors provided effective pathways to drain deep-sourced kimberlite and related magmas during supercontinent cycles. England and Houseman (1984) proposed that periods of strong kimberlite magmatic activity in North America and Africa during the Phanerozoic correlate with the slowest respective plate motions. However, the improved paleomagnetic and geochronological database for Africa suggests the opposite; that is, prominent peaks in kimberlite magmatic activity at 140–130 Ma and 100–80 Ma correspond to periods of fast acceleration of the African tectonic plate during Pangea breakup (Fig. 8).
Planation surfaces as a record of mantle dynamics: The case example of Africa
2018, Gondwana ResearchSynchroneity of cratonic burial phases and gaps in the kimberlite record: Episodic magmatism or preservational bias?
2015, Earth and Planetary Science LettersThe Cameroon Line: Analysis of an intraplate magmatic province transecting both oceanic and continental lithospheres: Constraints, controversies and models
2014, Earth-Science ReviewsCitation Excerpt :A regional pattern of topographic and bathymetric swells and irregularly shaped basins has long been a recognized peculiarity of the African plate (Holmes, 1944; Nyblade and Robinson, 1994; Burke, 1996; Doucouré and de Wit, 2003; Fig. 1a). Many researchers have interpreted this to reflect shallow-upper mantle convection (e.g., Burke and Wilson, 1972; McKenzie and Weiss, 1975; England and Houseman, 1984). However, the resolution of the present tomographic images of upper mantle and lithosphere variations across Africa is not yet of a quality to confidently model the effects of the mantle in dynamically supporting topography (e.g., Fishwick and Bastow, 2011; Raveloson et al., in press).