Progress in earth and planetary science 1

• Material Type: 電子書籍・電子雑誌
• Title: Progress in earth and planetary science
• Volume: 1
• Author/Editor: the Japan Geoscience Union
• Publication, Distribution, etc.: 日本 : Springer science+business media
• Publication Date: 2014
• Publication Date (W3CDTF): 2014
• ISSN (Periodical Title): 2197-4284
• ISSN-L (Periodical Title): 2197-4284
• Text Language Code: eng
• Persistent ID (NDL): info:ndljp/pid/8752522; https://dl.ndl.go.jp/pid/8752522
• Collection (particular): 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他; https://dl.ndl.go.jp/collections/B00035
• Acquisition Basis: オンライン資料収集制度
• Date Accepted (W3CDTF): 2014-09-25T20:21:39+09:00
• Access Restrictions: 国立国会図書館内限定公開
• Service for the Digitized Contents Transmission Service: 図書館・個人送信対象外
• Availability of remote photoduplication service: 不可
• Periodical Title (Persistent ID (NDL)): info:ndljp/pid/8752521; https://dl.ndl.go.jp/pid/8752521
• Data Provider (Database): 国立国会図書館 : 国立国会図書館デジタルコレクション; https://dl.ndl.go.jp

Table of Contents

Natural moissanite (SiC) : a low temperature mineral formed from highly fractionated ultra-reducing COH-fluids

An observation campaign of precipitable water vapor with multiple GPS receivers in western Java, Indonesia

The role of snowmelt runoff on the ocean environment and scallop production in Funka Bay, Japan

Heavy metal pollution in Ancient Nara, Japan, during the eighth century

Modeling in Earth system science up to and beyond IPCC AR5

A numerical experiment on the formation of the tropopause inversion layer associated with an explosive cyclogenesis : possible role of gravity waves

Shaking conditions required for flame structure formation in a water-immersed granular medium

Response of the mesosphere-thermosphere- ionosphere system to global change : CAWSES-II contribution

Typhoon-induced sea surface cooling during the 2011 and 2012 typhoon seasons : observational evidence and numerical investigations of the sea surface cooling effect using typhoon simulations

Invitation to progress in earth and planetary science

Water-melt interaction in hydrous magmatic systems at high temperature and pressure

Mechanism of long-standing Cenozoic basin formation in central Hokkaido : an integrated basin study on an oblique convergent margin

Coseismic visibility of a small fragile patch involved in the rupture of a large patch : implications from fully dynamic rate-state earthquake sequence simulations producing variable manners of earthquake initiation

Observations of GPS scintillation during an isolated auroral substorm

Distribution of U and REE on colloids in granitic groundwater and quality-controlled sampling at the Mizunami underground research laboratory

Structure and properties of forsterite-MgSiO3 liquid interface : molecular dynamics study

Contrasting partition behavior of F and Cl during hydrous mantle melting : implications for Cl/F signature in arc magmas

The Non-hydrostatic Icosahedral Atmospheric Model : description and development

Installing artificial macropores in degraded soils to enhance vertical infiltration and increase soil carbon content

Direct comparison of site-specific and basin-scale denudation rate estimation by in situ cosmogenic nuclides : an example from the Abukuma Mountains, Japan

Hydrothermal system in the Tatun Volcano Group, northern Taiwan, inferred from crustal resistivity structure by audio-magnetotellurics

Correction : invitation to progress in earth and planetary science

What is the solar influence on climate？ : Overview of activities during CAWSES-II

Lg wave propagation in the area around Japan : observations and simulations

Short-term slow slip events along the Ryukyu Trench, southwestern Japan, observed by continuous GNSS

Preface to the first volume of PEPS

Invitation to “Progress in earth and planetary science (PEPS)” by Japan geoscience union

Theoretical constraints of physical and chemical properties of hydrothermal fluids on variations in chemolithotrophic microbial communities in seafloor hydrothermal systems

Earthquake faulting in subduction zones : insights from fault rocks in accretionary prisms