Use of SMS texts for facilitating access to online alcohol interventions: a feasibility study

A41 Use of SMS texts for facilitating access to online alcohol interventions: a feasibility study In: Addiction Science & Clinical Practice 2017, 12(Suppl 1): A4

Japan Digital Elevation Model [DEM]

For the Regional Systems Analysis of Japan, the GTOP0 30 arc second resolution data tiles were projected into Lambert Comformal Conic projection using Clarke 1866 datum, with units in meters. The details for this are: Units: meters Central meridian: 135 E Standard parallel #1: 39 N Standard parallel #2: 27 N Latitude of origin: 33 N Datum: Clarke 1866 Cell size: 846 m Subsequently the DEM tiles were trimmed to the islands of Japan (including Hokkaido and the Senkyaku Chain) and reprojected into a Geographic Coordinate System decimal degrees WGS-84 version. The cell size in decimal degrees of the distributed WGS-84 version is 0.010215556

Japan-G Dataset, Gun and Kuni Maps (1887)

Gun sketch maps digitized from Kyudaka kyuryo torishirabecho 旧高旧領取調帳 by Motoi Kimura 木村礎. 205 Attributes, primarily historical variables and analytical derived variables. Original data does not include Hokkaido. (updated version includes completed Kuni maps, including Hokkaido). Compilers: Tsunetoshi Mizoguchi, G. W illiam Skinner, Catherine Koehler, Kyle Matoba, and Mark Henderson. Editors: Merrick Lex Berman, Fabian Drixler, and Akihiro Tsukamoto

Tectonic model for development of the Byrd Glacier discontinuity and surrounding regions of the Transantarctic Mountains during Neoproterozoic-Early Paleozoic

The Byrd Glacier discontinuity us a major boundary crossing the Ross Orogen, with crystalline rocks to the north and primarily sedimentary rocks to the south. Most models for the tectonic development of the Ross Orogen in the central Transantarctic Mountains consits of two-dimensional transects across the belt, but do not adress the major longitudinal contrast at Byrd Glacier. This paper presents a tectonic model centering on the Byrd Glacier discontinuity. Rifting in the Neoproterozoic producede a crustal promontory in the craton margin to the north of Byrd Glacier. Oblique convergence of the terrane (Beardmore microcontinent) during the latest Neroproterozoic and Early Cambrian was accompanied by subduction along the craton margin of East Antarctica. New data presented herein in the support of this hypothesis are U-Pb dates of 545.7 ± 6.8 Ma and 531.0 ± 7.5 Ma on plutonic rocks from the Britannia Range, subduction stepped out, and Byrd Glacier. After docking of the terrane, subduction stepped out, and Byrd Group was deposited during the Atdabanian-Botomian across the inner margin of the terrane. Beginning in the upper Botomian, reactivation of the sutured boundaries of the terrane resulted in an outpouring of clastic sediment and folding and faulting of the Byrd Group