Results 81 to 90 of about 1,707 (195)
Thermochemical Controls on the X, 410, and 660 Discontinuities in the Central Mediterranean
Abstract The mantle beneath the Central Mediterranean is thermally and compositionally heterogeneous, as indicated by fragmented and locally stagnant slabs in tomographic images and HIMU‐like anorogenic magmatism. Mantle discontinuities are sensitive to both temperature and composition, and thus provide a way to quantify these heterogeneities.
Luciana Bonatto +4 more
wiley +1 more source
Double volcanic tracks at Hawaii caused by bridgmanite-enriched primordial mantle blobs
Mantle plumes, rising from Earth’s deep interior, are expected to produce a single age-progressive hotspot track. However, Hawaiian volcanoes younger than ~7 million years form two subparallel volcanic chains, the Loa and Kea trends. The mechanism behind
Hao Liu +5 more
doaj +1 more source
Comparing Monte Carlo Models of Impact Alteration of Planetary Atmospheres
Abstract One process that affects atmospheric surface pressure is impact bombardment. The evolution of a planet's atmosphere under impact bombardment is an open question. We use a Monte Carlo method to evolve a range (0.006–92.5 bar) of initial atmospheres at Mars, Earth, and Venus under bombardment of 5×106 $5\times 1{0}^{6}$ impactors using seven ...
M. R. Huffman +4 more
wiley +1 more source
Thermal anomalies within the lithosphere are an important manifestation of mantle plume–lithosphere interaction. Early studies primarily concentrated on the presence of the Hainan plume and its surface responses, with comparatively little research ...
Huihui Zhang, Lijuan He, Yaqi Wang
doaj +1 more source
Abstract The Rio Grande Rise (RGR) is a major submarine feature in the South Atlantic that plays an important role in regional oceanographic dynamics. This study presents new U‐Pb geochronology of sedimentary rocks from the RGR, offering direct age constraints on carbonate and apatite embedded within Fe‐Mn crusts and associated foraminifera fossils ...
Giovanna Orletti Del Rey +8 more
wiley +1 more source
Inversion by Intrusion: Magma‐Driven Shortening in the Turkana Rift (East Africa)
Abstract Late Pliocene to Pleistocene inversion in the Turkana Rift, observed on seismic reflection data and in outcrop, presents a tectonic paradox by indicating local shortening in an overall extensional setting. Previous studies attributed this inversion either to the reactivation of obliquely oriented structural weaknesses or to reorientation of ...
Ameha A. Muluneh +6 more
wiley +1 more source
The link between mantle plumes and the formation of large igneous provinces (LIPs) is well established although the anatomy of these remains equivocal. Recent experimental studies and geophysical data suggest that the mantle plume head is more likely to ...
Hongbo Li +9 more
doaj +1 more source
Abstract An audiomagnetotelluric (AMT) survey was conducted within the Alto Paranaíba Igneous Province, southeastern Brazil, to delineate shallow occurrences of kamafugite, a rare ultrapotassic volcanic rock worldwide. A dense grid of AMT stations was deployed, allowing the construction of a high‐resolution 3D electrical resistivity model ...
Lucca M. Franco +6 more
wiley +1 more source
Non-mantle-plume process caused the initial spreading of the South China Sea. [PDF]
Yu X, Liu Z.
europepmc +1 more source
Dynamics of mantle plumes [PDF]
Mantle plumes are a link between different scales in the Earth’s mantle: They are an important part of large-scale mantle convection, transporting material and heat from the core-mantle boundary to the surface, but also affect processes on a smaller scale, such as melt generation and transport and surface magmatism.
openaire

