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10篇 您的检索式：作者名="Morgan Dale"

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		题名	作者	年代	出处	被引量
	1	Effects of porosity and clay content on wave velocities in sandstones显示文摘	HAN De-hua NUR A MORGAN Dale	1986	Geophysics1986，51，11：	1
	2	Effects of Porosity and Clay Content on Wave Velocities in Sandstones显示文摘	Han D H Nut A Morgan Dale	1986	Geophysics1986，51，11：	1
	3	Effects of porosity and clay content on wave velocities in sandstones 显示文摘	Han Dehua Nur A Morgan Dale	1986	Geophysics1986，51，11：	1
	4	Location robusmess of earthquakes in Sichuan Province, China 显示文摘	Sun Y Sadi Kuleli F Dale Morgan	2004	Seismological Research Letters2004，75，1：	1
	5	GAME ( Goals - Activity - Motor Enrichment) : protocol of a single blind randomised controlled trial of motor training, parent education and environmental enrichment for infants at high risk of cerebral palsy显示文摘	Morgan C Novak I Dale RC	2014	BMC Neural2014，14，：	1
	6	Effects of porosity and ealy content on wave velocities in sandstone显示文摘	Han Dehua Nur A Morgan Dale	1986	Geophysics1986，51，11：	1
	7	Optimising motor learning in infants at high risk of cerebral palsy: a pilot study显示文摘	Morgan C Novak I Dale R C	2015	BMC Pediatrics2015，15，1：	1
	8	Effects of porosity and clay content on wave velocities in sandstones显示文摘	Jan Dehua Nur A Morgan Dale	1986	Geophysics1986，51，11：	1
	9	BMP8B Increases Brown Adipose Tissue Thermogenesis through Both Central and Peripheral Actions显示文摘	Andrew J. Whittle Stefania Carobbio Luís Martins Marc Slawik Elayne Hondares María Jesús Vázquez Donald Morgan Robert I. Csikasz Rosalía Gallego Sergio Rodriguez-Cuenca Martin Dale Samuel Virtue Francesc Villarroya Barbara Cannon Kamal Rahmouni Miguel Lóp	2012	Cell2012，，4：	1
	10	Depth determination of the Moho interface beneath the Tibetan plateau and other areas of China显示文摘We apply the adaptive moving window method of Sun et al. to the most recent catalog data and the data recorded by portable stations to construct the velocity structure of the crust and upper mantle, and to determine the depth of the Moho interface beneath the Tibetan plateau and other areas of China. We first select 2 600 locations in the study region with 1 intervals, then at each location invert for a five-layer 1-D P-wave velocity model from the surface down to the uppermost mantle by performing a Monte Carlo random search. The Moho depth at each location is then determined, and the Moho interface beneath the study region is obtained through proper interpolation with certain smoothing. Compared to depths obtained by previous studies, our results show more accurate Moho depths in the Tibetan plateau, Tianshan region and other areas of the study region.	Youshun Sun Diming Yu M Nafi Toksz F Dale Morgan Xiyu Wang Jinrong Su Jun Liu	2012	Earthquake Science2012，25，5：	0

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