Introduction to the special volume on the Izu–Bonin – Mariana arc system     

Robert J. Stern  & Makoto Arima 《Island Arc》1998,7(3):295-300

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Characteristics of 3-dimensional earthquake ground motions     

Joseph Penzien  Makoto Watabe 《地震工程与结构动力学》1974,3(4):365-373

An orthogonal set of principal axes is defined for earthquake ground motions along which the component variances have maximum, minimum and intermediate values and the covariances equal zero. Corresponding axes are defined which yield maximum values for the covariances. The orthogonal transformations involved are identical in form to those used in the transformation of stress. Examination of real accelerograms reveals that the major principal axis points in the general direction of the epicentre and the minor principal axis is nearly vertical. It is concluded that artificially generated components of ground motion need not be correlated statistically provided they are directed along a set of principal axes.  相似文献   

Thermal-chemical instability in a pre-galactic gas cloud     

Yutaka Sabano  Makoto Tosa 《Astrophysics and Space Science》1986,119(1):167-168

The growth of thermal-chemical instability in a pre-galactic medium is followed by numerical simulation of gas dynamics. Results show that a primordial gas cloud breaks into self-gravitating subcondensations with the mass of normal stars.Paper presented at the IAU Third Asian-Pacific Regional Meeting, held in Kyoto, Japan, between 30 September–6 October, 1984.  相似文献   

Cosmological and astrophysical neutrino mass measurements     

K.N. AbazajianE. Calabrese  A. CoorayF. De Bernardis  S. Dodelson  A. FriedlandG.M. Fuller  S. HannestadB.G. Keating  E.V. Linder  C. LunardiniA. Melchiorri  R. Miquel  E. PierpaoliJ. Pritchard  P. SerraM. Takada  Y.Y.Y. Wong 《Astroparticle Physics》2011,35(4):177-184

Cosmological and astrophysical measurements provide powerful constraints on neutrino masses complementary to those from accelerators and reactors. Here we provide a guide to these different probes, for each explaining its physical basis, underlying assumptions, current and future reach.  相似文献   

Application of multi-isotope ratios to study the source and quality of urban groundwater in Metro Manila,Philippines   总被引：1，自引：0，他引：1  

Takahiro Hosono  Fernando Siringan  Tsutomu Yamanaka  Yu Umezawa  Shin-ichi Onodera  Takanori Nakano  Makoto Taniguchi 《Applied Geochemistry》2010

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A search for extragalactic H₂O maser emission towards IRAS galaxies – II. Discovery of an H₂O maser in the type 1 Seyfert galaxy NGC 4051     

Yoshiaki Hagiwara  Philip J. Diamond  Makoto Miyoshi  Emmanouel Rovilos  Willem Baan 《Monthly notices of the Royal Astronomical Society》2003,344(4):L53-L57

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Current-to-Current Converter for Scientific Underwater Cable Networks     

Asakawa  K. Kojima  J. Muramatsu  J. Takada  T. Kawaguchi  K. Mikada  H. 《Oceanic Engineering, IEEE Journal of》2007,32(3):584-592

A new current-to-current converter, which is a key device to branch a constant direct current (DC) into two constant DCs, was proposed [K. Asakawa , Proc. OCEANS, pp. 1868-1873, 2003]. It has been verified, through computer simulations and experiments using prototypes, to have good conversion efficiency and stable operation. Because the basic circuit is simple, high reliability is expected. The current-to-current converter is a key device to realize a constant current (CC) power-feeding system for scientific underwater cable networks having mesh topology, which is necessary to enhance robustness against cable breakdowns and to deploy sensors in 2-D and efficiently over a vast research area.  相似文献   

Petrogenesis of the new lherzolitic shergottite Grove Mountains 99027: Constraints of petrography,mineral chemistry,and rare earth elements     

Yangting Lin  Yunbin Guan  Daode Wang  Makoto Kimura  Laurie A. Leshin 《Meteoritics & planetary science》2005,40(11):1599-1619

Abstract— We report petrography, mineral chemistry, and microdistribution of rare earth elements (REE) in a new lherzolitic shergottite, Grove Mountains (GRV) 99027. The textural relationship and REE patterns of minerals suggest precipitation of cumulus olivine and chromite, followed by equilibrium crystallization of a closed system with a bulk composition of the inferred intercumulus melt. Subsolidus equilibrium temperatures of pyroxenes and olivine range from 1100 to 1210 °C, based on a two‐pyroxene thermometry and Ca partitioning between augite and olivine. Oxygen fugacity of the parent magma is 1.5–2.5 (av. 2.0 ± 0.4) log units below the quartz‐fayalite‐magnetite (QFM) buffer at 960–1360 °C, according to the olivine‐orthopyroxene‐chromite barometer. The ilmenite‐chromite barometer and thermometer show much wider ranges of oxygen fugacity (1.0–7.0 log unit below QFM) and temperature (1130–480 °C), suggesting subsolidus equilibration of the oxides at low temperatures, probably due to deep burial of GRV 99027 on Mars. The low oxygen fugacity and LREE depletion of the parent magma of GRV 99027 suggest low contamination by martian crust. Characteristics of GRV 99027 demonstrate similarity of lherzolitic shergottites, suggesting a high possibility of launch pairing or a homogeneous upper mantle of Mars if they were ejected by individual impact events. However, GRV 99027 probably experienced severe post‐shock thermal metamorphism in comparison with other lherzolitic shergottites, based on the re‐crystallization of maskelynite, the homogeneity of minerals, and the low subsolidus equilibrium temperatures between chromite and ilmenite.  相似文献   

Periodic ab initio Hartree-Fock study of trigonal and orthorhombic phases of boric oxides     

Akira Takada  C. R. A. Catlow  G. D. Price  C. L. Hayward 《Physics and Chemistry of Minerals》1997,24(6):423-431

The structure and electronic properties of trigonal and orthorhombic boric oxide (B₂O₃) are studied using periodic ab initio Hartree-Fock method. The optimised structural parameters for two B₂O₃ polymorphs are in good agreement with experimental data. The analyses of their electronic structures provide insights into the chemical nature of the B–O bond and the way in which it changes with the coordination number around boron and oxygen. Our quantum-chemical study suggests that the orthorhombic form is more ionic than the trigonal form and that the coordination number of boron around oxygen plays a more dominant role than that of oxygen around boron in B₂O₃ crystals.  相似文献   

The comoving-frame equation of radiative transfer in a curvilinear coordinate system     

Naboru Kaneko  Kazuhiko Morita  Makoto Maekawa 《Astrophysics and Space Science》1984,107(2):333-346

The comoving-frame equation of radiative transfer and moment equations are derived in orthogonal, curvilinear coordinates, inclusive of terms of orderv/c. The equation of radiative transfer, which contains the terms due to the effect of curvature of coordinate lines explicitly as well as those of Doppler shift and aberration, is the generalization of Castor's equation for spherical symmetry and of Buchler's equation for Cartesian coordinates. The moment equations agree with Buchler's.  相似文献