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Format
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Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Congo (1)
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West Congo Belt (1)
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Congo Craton (1)
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East Africa
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Lake Turkana (1)
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Zambia (1)
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East African Lakes
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Lake Turkana (1)
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Southern Africa
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Barberton greenstone belt (1)
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Kalahari Craton (1)
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South Africa
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Bushveld Complex (2)
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Mpumalanga South Africa (1)
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Transvaal region (1)
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West Africa
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Cameroon (1)
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Arctic region
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Greenland
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West Greenland (1)
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Asia
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Central Asia
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Kazakhstan
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Far East
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China
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Liaoning China
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Europe
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lead (2)
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silicon (9)
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fossils
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geochronology methods
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upper Precambrian
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igneous rocks
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sorosilicates
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Primary terms
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absolute age (1)
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Africa
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Central Africa
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Congo (1)
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West Congo Belt (1)
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Congo Craton (1)
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East Africa
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Lake Turkana (1)
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Zambia (1)
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East African Lakes
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Lake Turkana (1)
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Southern Africa
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Barberton greenstone belt (1)
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South Africa
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Bushveld Complex (2)
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Transvaal region (1)
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-
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West Africa
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Cameroon (1)
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-
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Arctic region
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Greenland
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Isua Belt (1)
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asbestos deposits (1)
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Asia
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Central Asia
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Kazakhstan
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Kokchetav Kazakhstan (1)
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-
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Far East
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China
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Chongqing China (1)
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Dabie Mountains (1)
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Guangxi China (1)
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Liaoning China
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Haicheng China (1)
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Sulu Terrane (1)
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Japan
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Kyushu
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Kagoshima Japan (1)
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Vietnam (1)
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Indian Peninsula
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India
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Jharkhand India
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Madhya Pradesh India (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
talc
Formation of talc in the subduction interface: Mg isotopes demonstrate Mg loss over Si gain Open Access
Mineralogical and geochemical facets of the massive deposition of stibnite-metastibnite at a seafloor hydrothermal field (Wakamiko Crater, Kagoshima Bay, Ryukyu Volcanic Arc) Available to Purchase
Thermal Decomposition Kinetics of Clinochlore at High Temperature and Its Implications Available to Purchase
The role of H 2 O in the deformation and microstructural evolution of the upper mantle Open Access
In this chapter, we evaluate how the incorporation of H 2 O as a thermodynamic component influences phase relations in a peridotite composition. This component – present either in the form of hydrous minerals, aqueous fluids and hydrous melts, or as a structurally-bonded trace element at defect sites of nominally anhydrous minerals (NAMs) – may influence upper-mantle rheology in diverse ways. By presenting various natural cases, we identify key incorporation mechanisms and assess their role in the microstructural evolution of ultramafic rocks at different depths in the Earth’s interior. These data suggest that the influence of either aqueous fluids or hydrous melts on rheology out-matches that of NAMs or stable hydrous phases across much of the lithospheric mantle. Consequently, future research is expected to shift towards a better understanding of the transient conditions in the lithosphere that control the availability and transport of aqueous fluids and hydrous melts. These transient conditions are likely to play a more dominant role than the sole ability of hydrous defects in NAMs – a role that is currently less well-constrained experimentally – in controlling the ductile deformation of the upper mantle.