Results 141 to 150 of about 2,132,735 (177)

The effects of local variations in conditions on carbon storage and release in the continental mantle. [PDF]

Natl Sci Rev
Foley SF, Chen C, Jacob DE.
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A novel approach for studying lithospheric deformation driven by asthenospheric flow

Krstekanic N, Willingshofer E, Auzemery A, Matenco L, Smits J.   +4 more
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Thermal Evolution of the Lithosphere‐Asthenosphere Boundary Beneath Arc and Its Geodynamic Implications: Depth Variation of Thermal Histories of Mantle Xenoliths From Ichinomegata, Northeast Japan

Journal of Geophysical Research - Solid Earth, 2023
Quantitative reconstruction of thermal history recorded in mantle xenoliths is imperative for understanding the temporal change of thermal state and dynamics of the lithosphere‐asthenosphere boundary (LAB).
Yuto Sato, K. Ozawa
semanticscholar   +1 more source

Equilibration Depth and Temperature of Neogene Alkaline Lavas in the Cordillera of Alaska and Canada as a Constraint on the Lithosphere-Asthenosphere Boundary

Canadian journal of earth sciences (Print), 2023
We have estimated the geochemical equilibration depth and temperature of the widespread Neogene alkaline basalts in the Cordillera of Alaska, NW Canada and in Mexico using geobarometry on bulk compositions that have been minimally differentiated in ...
D. Canil, R. Hyndman
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Hygrometric Control on the Lithosphere‐Asthenosphere Boundary: A 28 Million Year Record From the Canadian Cordillera

Geophysical Research Letters, 2021
The depth to the lithosphere‐asthenopshere boundary (LAB) provides a strong control on the temperature and strength of the lithosphere and its susceptibility to tectonic deformation.
D. Canil, R. Hyndman, Dominic Fode
semanticscholar   +1 more source

The lithosphere-asthenosphere boundary and lithosphere replacement as informed by mantle xenoliths and their host lavas

Canadian journal of earth sciences (Print)
Alkaline lavas hosting mantle xenoliths occur in the hot back arc of the Cordillera of western Canada and Alaska and provide constraints on lithosphere thickness (within 5 to 10 km) and controls on the lithosphere-asthenosphere boundary (LAB).
D. Canil
semanticscholar   +1 more source

Petrogenesis of end-Cretaceous/Early Eocene lamprophyres from the Deccan Large Igneous Province: Constraints on plume-lithosphere interaction and the post-Deccan lithosphere-asthenosphere boundary (LAB) beneath NW India

Lithos, 2019
We present petrology, geochemistry and radiogenic isotope (Sr and Nd) data of thirteen post-Deccan lamprophyre dykes in the Narmada rift zone from the Chhotaudepur alkaline province of the Deccan Large Igneous Province (DLIP).
R. Pandey, Ashutosh Pandey, N. V. C. Rao, B. Belyatsky, A. Choudhary, B. Lehmann, D. Pandit, P. Dhote   +7 more
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A plume origin for hydrous melt at the lithosphere–asthenosphere boundary

Nature, 2022
D. Blatter, S. Naif, K. Key, A. Ray
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Amphibole stability, water storage in the mantle, and the nature of the lithosphere-asthenosphere boundary

Earth and Planetary Science Letters, 2023
M. Putak Juriček, H. Keppler
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Undulating electrical lithosphere–asthenosphere boundary beneath Northeast China; as revealed by long–period magnetotelluric data

Tectonophysics, 2023
Zikun Zhou, Deli Wang, Tianqi Wang, A. Weng, Yabin Li, Junhao Guo, Xueqiu Wang   +6 more
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