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- W89701458 abstract "Introduction: The interpretation of geophysical datasets reflects remote responses to the physical properties of Earth’s interior at the present day. Translating this information into actualistic Earth models requires input from petrological and geochemical observations and measurements using tangible samples of the deepearth materials. In recent years exciting new tools, collectively termed 4-D Lithosphere Mapping [1], have been sequentially developed to track the evolution of lithospheric mantle, based on the integration of geochemical and petrophysical properties of mantlederived materials with tectonic syntheses and geophysical datasets. This methodology can provide some important constraints on fundamental questions such as the compositional structure of sub-continental lithospheric mantle (SCLM) formed at different times, the lateral variability of SCLM composition and its effects on tectonics, and the extent to which lithospheric mantle can be recycled into the convecting mantle, or is irreversibly differentiated from it. One of the most important results has been the demonstration (quantified using a large database of xenolith and garnet and chromite xenocryst compositions) that the composition of the SCLM varies in a systematic way correlated with the age of the last major tectonothermal event in the overlying crust (lower MgO and higher CaO and Al2O3 with decreasing age) [2]." @default.
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- W89701458 date "2001-05-01" @default.
- W89701458 modified "2023-10-01" @default.
- W89701458 title "Geochemical Remote Sensing of the Deep Earth: Tales of Longevity, Transformation and Destruction" @default.
- W89701458 hasPublicationYear "2001" @default.
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