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Deep continental roots and cratons
The formation and preservation of cratons—the oldest parts of the continents, comprising
over 60 per cent of the continental landmass—remains an enduring problem. Key to craton …
over 60 per cent of the continental landmass—remains an enduring problem. Key to craton …
The bio-chemical cycle of iron and the function induced by ZVI addition in anaerobic digestion: A review
Zero-valent iron (ZVI) is known to be an additive in facilitating waste treatment and improving
biogas production in anaerobic digestion (AD) systems. This review concentrates on the …
biogas production in anaerobic digestion (AD) systems. This review concentrates on the …
Identification of source lithology in the Hawaiian and Canary Islands: Implications for origins
Results are reported of an exploration of mantle source lithology for intraplate magmas
using whole-rock and olivine phenocryst compositions. This analysis includes modern mid …
using whole-rock and olivine phenocryst compositions. This analysis includes modern mid …
An olivine-free mantle source of Hawaiian shield basalts
More than 50 per cent of the Earth's upper mantle consists of olivine and it is generally
thought that mantle-derived melts are generated in equilibrium with this mineral. Here …
thought that mantle-derived melts are generated in equilibrium with this mineral. Here …
The rapid drift of the Indian tectonic plate
The breakup of the supercontinent Gondwanaland into Africa, Antarctica, Australia and India
about 140 million years ago, and consequently the opening of the Indian Ocean, is thought …
about 140 million years ago, and consequently the opening of the Indian Ocean, is thought …
Ambient and excess mantle temperatures, olivine thermometry, and active vs. passive upwelling
Mantle temperatures provide a key test of the mantle plume hypothesis, and olivine-liquid
equilibria provide perhaps the most certain means of estimating mantle temperatures. Here …
equilibria provide perhaps the most certain means of estimating mantle temperatures. Here …
The lithosphere-asthenosphere boundary
Seismological models of upper-mantle structure are providing new constraints on the
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …
Seismic evidence for significant lateral variations in lithospheric thickness beneath the central and western North China Craton
We have migrated teleseismic S-receiver functions to construct detailed lithospheric
structure images that cover the three constituent parts of the North China Craton (NCC). Our …
structure images that cover the three constituent parts of the North China Craton (NCC). Our …
The nature of the lithosphere‐asthenosphere boundary
Plate tectonic theory was developed 50 years ago and underpins most of our understanding
of Earth's evolution. The theory explains observations of magnetic lineations on the seafloor …
of Earth's evolution. The theory explains observations of magnetic lineations on the seafloor …
The elusive lithosphere–asthenosphere boundary (LAB) beneath cratons
The lithosphere–asthenosphere boundary (LAB) is a first-order structural discontinuity that
accommodates differential motion between tectonic plates and the underlying mantle …
accommodates differential motion between tectonic plates and the underlying mantle …