Modern-style plate subduction preserved in the Palaeoproterozoic West African craton

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Lithospheric thickness records tectonic evolution by controlling metamorphic conditions

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Chapter 34: The Paleoproterozoic (Rhyacian) Gold Deposits of West Africa

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The controls on the thermal evolution of continental mountain ranges

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Local Rapid Exhumation and Fast Cooling in a Long-lived Paleoproterozoic Orogeny

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Pressure and Temperature Estimation in Greenschist‐Facies Metapelites: An Example From the Variscan Belt in Sardinia

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The Logoualé Band: A large Archean crustal block in the Kenema-Man domain (Man-Leo rise, West African Craton) remobilized during Eburnean orogeny (2.05 Ga)

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Zircon Trace Element Constraints on the Evolution of the Paleoproterozoic Birimian Granitoids of the West African Craton (Ghana)

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Experimental modeling of mantle metasomatism coupled with eclogitization of crustal material in a subduction zone

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Onset of the supercontinent cycle: Evidence for multiple oceanic arc accretion events in the Paleoproterozoic Sefwi Greenstone Belt of the West African Craton

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Precambrian supercontinents and supercycles—an overview

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Influence of Deformation and Fluids on Ti Exchange in Natural Quartz

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From subduction initiation to hot subduction: Life of a Neoarchean subduction zone from the Dengfeng Greenstone Belt, North China Craton

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Geochronology and geochemistry of 2.3 Ga mafic intrusions in the Dengfeng area: Evidence for early Paleoproterozoic subduction in the southern North China Craton

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Strike-slip metamorphic core complexes: Gneiss domes emplaced in releasing bends

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Chemical and boron isotope composition of tourmaline from the Kiaka orogenic gold deposit (Burkina Faso, West African Craton) as a proxy for ore-forming processes

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Juxtaposition of diverse, subduction-related tectonic blocks with contrasting metamorphic features and ages in the Paleoproterozoic Aketashitage orogen, NW China: Implications for Precambrian orogeny

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The stability of subducted glaucophane with the Earth’s secular cooling

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Evidence for late Proterozoic subduction from 700-Myr-old blueschists in China

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Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time: Comment and Reply: REPLY

Stern, R. J. (2006) · Geology · doi:10.1130/g23026.1