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Relevant bibliographies by topics / Mid-lithospheric discontinuity

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Journal articles

Academic literature on the topic 'Mid-lithospheric discontinuity'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Mid-lithospheric discontinuity"

1

Tharimena, Saikiran, Catherine A. Rychert, and Nicholas Harmon. "Seismic imaging of a mid-lithospheric discontinuity beneath Ontong Java Plateau." Earth and Planetary Science Letters 450 (September 2016): 62–70. http://dx.doi.org/10.1016/j.epsl.2016.06.026.

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2

Goev, A. G. "Deep velocity structure of the eastern margin of the Sarmatian protocraton based on the «Aleksandrovka» seismic station data from the receiver function technique." Moscow University Bulletin. Series 4. Geology, no. 6 (February 6, 2023): 88–94. http://dx.doi.org/10.33623/0579-9406-2022-6-88-94.

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A velocity section was obtained to a depth of about 250 km on the eastern margin of the Sarmatia protocraton (East-European Craton) based on P receiver functions (PRF). Seismograms of the new broadband station «Aleksandrovka» were used as initial data. The section reveals the main seismic boundaries, and also shows the presence of mid-lithospheric discontinuity in the upper mantle (MLD).

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3

Kind, R., X. Yuan, J. Mechie, and F. Sodoudi. "Structure of the upper mantle in the north-western and central United States from USArray S-receiver functions." Solid Earth Discussions 7, no. 1 (2015): 1025–57. http://dx.doi.org/10.5194/sed-7-1025-2015.

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Abstract. We used more than 40 000 S-receiver functions recorded by the USArray project to study the structure of the upper mantle between the Moho and the 410 km discontinuity from the Phanerozoic western United States to the cratonic central US. We obtained clear observations of downward velocity reductions in the uppermost mantle which are commonly interpreted as the lithosphere-asthenosphere boundary (LAB) in the western US and as the mid-lithospheric discontinuity (MLD) in the cratonic US. We observe the western LAB reaching partly to the mid-continental rift system underneath the cratoni

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4

Kind, R., X. Yuan, J. Mechie, and F. Sodoudi. "Structure of the upper mantle in the north-western and central United States from USArray S-receiver functions." Solid Earth 6, no. 3 (2015): 957–70. http://dx.doi.org/10.5194/se-6-957-2015.

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Abstract. We used more than 40 000 S-receiver functions recorded by the USArray project to study the structure of the upper mantle between the Moho and the 410 km discontinuity from the Phanerozoic western United States to the cratonic central US. In the western United States we observed the lithosphere–asthenosphere boundary (LAB), and in the cratonic United States we observed both the mid-lithospheric discontinuity (MLD) and the LAB of the craton. In the northern and southern United States the western LAB almost reaches the mid-continental rift system. In between these two regions the craton

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5

Zhang, Yaoyang, Ling Chen, Yinshuang Ai, and Mingming Jiang. "Lithospheric structure beneath the central and western North China Craton and adjacent regions from S-receiver function imaging." Geophysical Journal International 219, no. 1 (2019): 619–32. http://dx.doi.org/10.1093/gji/ggz322.

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Summary To elucidate the nature and extent of the lithospheric modification in the central and western North China Craton (NCC) and adjacent regions, we used the wave equation–based migration technique of S-receiver function on teleseismic data collected from 314 broadband stations in this region to image the lithospheric structure. Incorporating data from previous lithospheric structure studies, we obtained unprecedented high-resolution depth maps of the lithosphere–asthenosphere boundary (LAB) and mid-lithospheric discontinuity (MLD) in the NCC. Our results show more detailed variations of t

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6

Smart, Katie A., Sebastian Tappe, Alan B. Woodland, Chris Harris, Loretta Corcoran, and Antonio Simonetti. "Metasomatized eclogite xenoliths from the central Kaapvaal craton as probes of a seismic mid-lithospheric discontinuity." Chemical Geology 578 (September 2021): 120286. http://dx.doi.org/10.1016/j.chemgeo.2021.120286.

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7

Shi, Ya-Nan, Fenglin Niu, Zhong-Hai Li, and Pengpeng Huangfu. "Craton destruction links to the interaction between subduction and mid-lithospheric discontinuity: Implications for the eastern North China Craton." Gondwana Research 83 (July 2020): 49–62. http://dx.doi.org/10.1016/j.gr.2020.01.016.

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8

Liu, Lin, Simon L. Klemperer, and Alexander R. Blanchette. "Western Gondwana imaged by S receiver-functions (SRF): New results on Moho, MLD (mid-lithospheric discontinuity) and LAB (lithosphere-asthenosphere boundary)." Gondwana Research 96 (August 2021): 206–18. http://dx.doi.org/10.1016/j.gr.2021.04.009.

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9

Saha, Sriparna, Rajdeep Dasgupta, and Kyusei Tsuno. "High Pressure Phase Relations of a Depleted Peridotite Fluxed by CO2 -H2 O-Bearing Siliceous Melts and the Origin of Mid-Lithospheric Discontinuity." Geochemistry, Geophysics, Geosystems 19, no. 3 (2018): 595–620. http://dx.doi.org/10.1002/2017gc007233.

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10

Peng, Ye, and Mainak Mookherjee. "Thermoelasticity of tremolite amphibole: Geophysical implications." American Mineralogist 105, no. 6 (2020): 904–16. http://dx.doi.org/10.2138/am-2020-7189.

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Abstract We investigated the structure, equation of state, thermodynamics, and elastic properties of tremolite amphibole [Ca2Mg5Si8O22(OH)2] up to 10 GPa and 2000 K, using first principles simulations based on density functional perturbation theory. We found that at 300 K, the pressure-volume results can be adequately described by a third-order Birch-Murnaghan equation of state with bulk moduli K0 of 78.5 and 66.3 GPa based on local density approximation (LDA) and generalized gradient approximation (GGA), respectively. We also derived its coefficients of the elastic tensor based on LDA and GGA

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