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First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquén Basin, Argentina
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Journal of the Geological Society, 167, 633-636, 21 June 2010, https://doi.org/10.1144/0016-76492010-025
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Zircon dating ties NE Atlantic sill emplacement to initial Eocene global warming
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Journal of the Geological Society, 167, 433-436, 19 April 2010, https://doi.org/10.1144/0016-76492009-125
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No need for lithospheric extension for exhuming (U)HP rocks by normal faulting
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Journal of the Geological Society, 167, 225-228, 1 March 2010, https://doi.org/10.1144/0016-76492009-134
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Spatial variations in biosphere ⁸⁷Sr/⁸⁶Sr in Britain
J.A. Evans, J. Montgomery, G. Wildman and N. Boulton

Journal of the Geological Society, 167, 1-4, 7 January 2010, https://doi.org/10.1144/0016-76492009-090
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The gravity fields of Palawan and New Caledonia: insights into the subsurface geometries of ophiolites
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Journal of the Geological Society, 166, 985-988, 28 October 2009, https://doi.org/10.1144/0016-76492009-067
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A magmatic age and four successive metamorphic events recorded in zircons from a single meta-anorthosite sample in the Central Zone of the Limpopo Belt, South Africa
H. Mouri, M.J. Whitehouse, G. Brandl and H.M. Rajesh

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Evidence for an early Archaean granite from Bastar craton, India
H.M. Rajesh, J. Mukhopadhyay, N.J. Beukes, J. Gutzmer, G.A. Belyanin and R.A. Armstrong

Journal of the Geological Society, 166, 193-196, 27 February 2009, https://doi.org/10.1144/0016-76492008-089
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Present-day stress and neotectonic provinces of the Baram Delta and deep-water fold–thrust belt
Rosalind C. King, Richard R. Hillis, Mark R.P. Tingay and Chris K. Morley

Journal of the Geological Society, 166, 197-200, 27 February 2009, https://doi.org/10.1144/0016-76492008-062R
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Orogenic versus extensional settings for regional metamorphism: Knoydartian events in the Moine Supergroup revisited
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Journal of the Geological Society, 166, 201-204, 27 February 2009, https://doi.org/10.1144/0016-76492008-015
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Degree of magnetic anisotropy as a strain-intensity gauge in a saturated finite-strain zone
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