They suggested that apparent resistivities depressed in all directions were responsible for unrealistically high mantle conductivities being inferred from 1D interpretations of long-period marine MT data. It is the only journal to be entirely devoted to the physical and chemical processes of planetary interiors. It is the only journal to be entirely devoted to the physical and chemical processes of planetary interiors. Geological settings and sampling Relics of the Tsunami generated by the 1755 Lisbon earthquake, magnitude 8.5–8.75 (e.g., Abe, 1979; Johnston, 1996), were found in the Algarve region, southern Portugal (Hindson and Andrade, 1999), in the estuary of the Boca do Rio (Fig. Besides, GRACE observations have improved our understanding of the Privacy Policy The scope of Physics of the Earth and Planetary Interiors covers Physics and Astronomy (miscellaneous) (Q1), Astronomy and Astrophysics (Q2), Geophysics (Q2), Space and Planetary Science (Q2) . 1A). https://doi.org/10.1016/j.pepi.2021.106654, https://doi.org/10.1016/j.pepi.2021.106652, https://doi.org/10.1016/j.pepi.2021.106651, https://doi.org/10.1016/j.pepi.2020.106638, https://doi.org/10.1016/j.pepi.2019.106325, High-pressure vibrational spectra of humite-group minerals: Fluorine effect on thermodynamic properties and hydrogen bonds, Erratum to “The influence of spreading rate and permeability on melt focusing beneath mid-ocean ridges” [Physics of the Earth and Planetary Interiors 304 (2020) 106486], 3-D time-domain electromagnetic modeling based on multi-resolution grid with application to geomagnetically induced currents, MAGLAB: A computing platform connecting geophysical signatures to melting processes in Earth's mantle, Extremely young melt infiltration of the sub-continental lithospheric mantle, Geller-Fest Workshop on Big Data in Geosciences: From Earthquake Swarms to Consequences of Slab Dynamics, Physical properties and observations of the lithosphere-asthenosphere system, Variations of the Earth’s magnetic field as revealed by archaeological baked clays: contribution of archaeomagnetism to geomagnetism and archaeology. Each trace is aligned to manually picked PKIKP (t=0). Channell / Physics of the Earth and Planetary Interiors 169 (2008) 140–151 Table 1 Location, water depth, length, sedimentation rate, normalizer, and estimated age for relative paleointensity records used in this study Records Location Water depth (m) Record length (m) Sedimentation rate (cm/kyr) Normalizer used Oldest age (Ma) References ODP 983 60.40N, 23.64W … / Physics of the Earth and Planetary Interiors 168 (2008) 71–87 73 Fig. (A) An example of PKIKP precursors and PKIKP/PKiKP phases observed at northern South America and the southeastern Caribbean. E-mail address: barbara@seismo.berkeley.edu (B. Romanowicz). Download PDF. A.F. / Physics of the Earth and Planetary Interiors 174 (2009) 24–32 29 finally note that our modeling involves a temperature-independent studies (up to 2 GPa) for a variety of crystal structures, including thermal diffusion coefficient which represents the averaged over our materials of study (g = 6–12) (Ross et al., 1984). / Physics of the Earth and Planetary Interiors 180 (2010) 179–188 (MgFe2O4), which is likely different from the more reduced con- ditions inferred for the lower mantle (e.g., Frost and McCammon, 2008). cCentre for Earth Evolution and Dynamics (CEED), University of Oslo, P.O. Gerd Steinle-neumann. In. The same setup can be used for the … Thus, when we look at the interior of the Earth from the surface, we are faced with a situation where clear indications of anisotropy could arise from intrinsic effects such as LPO, or be apparent, rep- Early models assumed flow in an isotropic medium dri-ven by temperature and density gradients (e.g. Karato / Physics of the Earth and Planetary Interiors 176 (2009) 83–88 85 Fig. On Earth, the elastic thickness is controlled by the depth of the 450°C isotherm (Watts, 1994). Download Free PDF. Copyright © 2021 Elsevier B.V. or its licensors or contributors. We would like to ask you for a moment of your time to fill in a short questionnaire, at the end of your visit. E.A. 3. Thomas et al. / Physics of the Earth and Planetary Interiors 176 (2009) 198–212 199 Fig. A short summary of this paper. If you wish to place a tax exempt order 2. d-Spacings vs. angle between the diffracting plane normal and the maximum stress axis at 49.3GPa. You may choose to submit your manuscript as a single Word or PDF file to be used in the refereeing process. We assume that each of Earth’s plates operates in either the sluggish-lid or the mobile-lid mode. Earth Planet. (2011), doi:10.1016/ j.pepi.2011.04.011. Original research papers, review articles, short communications and book reviews are all published on a regular basis; and from time to time special issues of the journal are devoted to the publication of the proceedings of symposia and congresses which the editors feel will be of particular interest to the reader. Inter.” . 1. We also take into consider-ation the relative contribution of the modes to the total surface Z.-X. This process releases In our particle-based method, the fineness field Ais represented by a distribution of particles. 3. Okal et al. Goncharov et al. 2. Launched in 1968 to fill the need for an international journal in the field of planetary physics, geodesy and geophysics, Physics of the Earth and Planetary Interiors has now grown to become important reading matter for all geophysicists. Paleointensity versus age for lunar samples (a) reproduced from Cisowski et al. / Physics of the Earth and Planetary Interiors 182 (2010) 113–118 115 Table 1a Unit-cell parameters and unit-cell volume for CaPtO3 at ambient pressure and temperature; the numbers in parentheses are estimated standard uncertainties and refer to the least-significant digits. 180 K. Otsuka et al. L. Dai, S.-i. / Physics of the Earth and Planetary Interiors 174 (2009) 159–164 was made. Squares indicate the first arrival of the PKIKP precursors estimated from a random scattering model. Monster et al. Thanks in advance for your time. By continuing you agree to the use of cookies. L. Miyagi et al. Ziegler et al. These are all of direct relevance for planetary accretion and differen-tiation processes (Stevenson, 1990), the time evolution of mantle and core temperatures (Stacey and Loper, 1984), and the gen- Besides, GRACE observations have improved our understanding of the (a) SMEAN shear wave velocity anomalies near the core–mantle boundary (Becker and Boschi, 2002), illustrating the location and lateral extent of the present African A. Wüstefeld et al. 142 C. Xuan, J.E.T. Tectonic setting Hainan island is located near the southeastern margin of the Eurasian plate, and has been affected by the motions and interac-tion of the Indian and Philippine Sea plates and by the extension of the South China Sea basin (Fig. Hager and O’Connell, 1981; Tackley, 1993; Bunge et al., 1996). They derive this expression using the variational perturbation method for hard spheres (Mansoori and Canfield, 1969). N. Saloor, E.A. Before mixing these material types into a larger com-pilation, results obtained from the different material types should be quantitatively compared. emplaced. First Previous Next Last (0/0) Start your review of [PHYSICS OF THE EARTH AND PLANETARY INTERIORS]: Your review informs others about the journal. Bull et al. Download PDF Package. Physics of the Earth and Planetary Interiors, established in October 1967, is a biweekly peer-reviewed scientific journal published by Elsevier. Free PDF. / Physics of the Earth and Planetary Interiors 180 (2010) 179–188 (MgFe2O4), which is likely different from the more reduced con-ditions inferred for the lower mantle (e.g., Frost and McCammon, 2008). Looking for an author or a specific volume/issue? M.W.L. a Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, MD 21218, USA bDepartment of Physics, University of Colorado, Boulder, CO 80309, USA article info Article history: Received 25 April 2012 Receivedin revised form20September 2012 Accepted 7 October 2012 Available online xxxx Edited by Chris Jones Keywords: Geodynamo Mantle convection Polarity reversals … Red (purple) values show areas with a high (low) Sofia Akber. 60 X. Zhang, H. Paulssen/Physics of the Earth and Planetary Interiors 192-193 (2012) 59–67. 54 L. Vocadlo et al. The Standard Abbreviation (ISO4) of Physics of the Earth and Planetary Interiors is “Phys. Standard Journal Abbreviation (ISO4) - Physics of the Earth and Planetary Interiors. Download Full PDF Package. T. Kidane et al. The scientific journal Physics of the Earth and Planetary Interiors is included in the Scopus database. J.N. Miller, F. Niu / Physics of the Earth and Planetary Interiors 170 (2008) 89–94 91 Fig. Thick solid lines is recalculated from the Rietveld refinement with C12 or C44 refined. A similar isotherm exists beneath the lunar lithosphere (Crosby and McKenzie, 2005). Physics of the Earth and Planetary Interiors: Phase Transformations and the Earth's Interior v. 3: Symposium Proceedings: Ringwood, A.E., Green, D. H.: Amazon.nl K. Lawrence et al. / Physics of the Earth and Planetary Interiors 174 (2009) 24–32 27 monochromator-spectrograph with CCD detector in UV–vis and by FT-IR spectrometer (Nicolet 750 Magna) equipped by a halo- gen lamp and a CaF2 beamsplitter for near IR spectral range. We are always looking for ways to improve customer experience on Elsevier.com. About Physics of The Earth and Planetary Interiors Launched in 1968 to fill the need for an international journal in the field of planetary physics, geodesy and geophysics, Physics of the Earth and Planetary … Personal information is secured with SSL technology. ScienceDirect ® is a registered trademark of Elsevier B.V. ScienceDirect ® is a registered trademark of Elsevier B.V. / Physics of the Earth and Planetary Interiors 170 (2008) 34–45 Fig. Box 1028 Blindern, N-0315 Oslo, Norway d GFZ German Research Centre for Geosciences, Telegraphenberg, D-14473 Potsdam, Germany e Mineral Physics Institute, Department of Earth and Space Sciences, Stony Brook University, Stony Brook, New York, USA A.S. Wolf, D.J. 1. Please click here for more information on our author services. Reviews on PHYSICS OF THE EARTH AND PLANETARY INTERIORS: Write a review: No reviews. experiment by adding a small amount of hydrochloric acid. University College London, London, United Kingdom Email Dr. ana Ferreira, PhD. Klemperer on 18 December 2007, but labels given here are original and used for reference in the text of this paper. Your Paper Your Way We now differentiate between the requirements for new and revised submissions. Earth Planet. please, Physics of the Earth and Planetary Interiors. 2.1. A. Lindsay-Scott et al. Mineral Physics of Earth and Planetary Interiors . 218 C. Beggan, K. Whaler / Physics of the Earth and Planetary Interiors 167 (2008) 217–222 one-norm minimisation inversion technique, initially imposing a minimumglobalroot-mean-square(RMS)flowvelocityconstraint. A number of experimental high-pressure techniques, including ultrasonic interferometry, nuclear resonant inelastic X-ray scatter-ing (NRIXS), high-energy resolution inelastic X-ray scattering Gerd Steinle-neumann. Physics of the Earth and Planetary Interiors 269 (2017) 58–90 Contents lists available at ScienceDirect Physics of the Earth and Planetary Interiors Physics of the Earth and Planetary Interiors 110 1999 83–93 . Physics of the Earth and Planetary Interiors 285 (2018) 76–90 77. here it is solved using a particle method (e.g., Tackley and King, 2003), similarly to how the compositional field is modeled in mantle convec-tion studies (McNamara and Zhong, 2004). Replacing (8) with (10) and adding the contribution of S-wave ra-diation at the source, the estimated energy EE is then defined as: = E +〈 〉q ∗ π F F ε 1 4 () E . Box 1028 Blindern, N-0315 Oslo, Norway d GFZ German Research Centre for Geosciences, Telegraphenberg, D-14473 Potsdam, Germany e Mineral Physics Institute, Department of Earth and Space Sciences, Stony Brook University, Stony Brook, New York, USA Angle between the diffracting plane normal and the southeastern Caribbean Zhong / Physics of the and. 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