نتایج جستجو برای: surficial geology

تعداد نتایج: 11614  

2006
Alan Rogerson

Modem geology was founded by James Hutton at the end of the 18th cenhuy as an observational, descriptive, qualitative, and subjective science. It was the pioneer work of Pearson (1901) and Spearman (1904) in statistics applied to agriculture, biology, medicine, and psychology, that led to the first major inroads of quantitative techniques in geology and the models they used were above all stati...

2013
R. Jaumann Stephan M. C. De Sanctis Garry D. Blewett

The Dawn spacecraft collected over 28,000 images and a wealth of spectral data of Vesta’s surface. These data enable analysis of Vesta’s diverse geology including impact craters of all sizes and unusual shapes, a variety of ejecta blankets, large troughs, impact basins, enigmatic dark material, and considerable evidence for mass wasting and surface alteration processes [1,2,3]. Two large impact...

2002
E. N. Church

pillow lavas are locally conspicuous. A unit consisting of dark, thinly bedded sandstone and siltstone, lccally ranging to several hundred feet thick, is lowermost in the exposed section. The middle division consists of about 3,500 feet of mixed andesi.:e and basalt volcaniclastic rocks ~ lahar, tuff breccia, volcanic sandstone, and conglomeratic beds which rest on relatively thin, fossiliferou...

Journal: :J. Symb. Log. 2016
Gunter Fuchs Ralf Schindler

One of the basic concepts of set theoretic geology is the mantle of a model of set theory V: it is the intersection of all grounds of V, that is, of all inner models M of V such that V is a set-forcing extension of M . The main theme of the present paper is to identify situations in which the mantle turns out to be a fine structural extender model. The first main result is that this is the case...

2005
Posas Hills

when the a particle is initially in the state i. The Sij's are determined from the relative intensity of the lines emitted in transition from that state. Take the particular case where S12 = S02 = 1/2 and (12 = #o2 = (01 1-7 13= 1/200 then P1/P2 = 4.3. This ratio is nearly the same as that of the internal conversion coefficient of y rays from RaC. There the values of this coefficient can be div...

Journal: :Journal of the Japan Society of Engineering Geology 2010

2008
Kyle K. Nichols

A Thesis Progress Report Presented By Kyle K. Nichols .to The Faculty of the Geology Department of The University of Vermont October 15, 1998 Accepted by the Faculty of the Geology Department, the University of Vermont, in partial fulfillment of the requirements for the degree of Master of Science specializing in Geology. The following members of the Thesis Committee have read and approved this...

2013
Valentí Rull Núria Cañellas-Boltà Alberto Sáez Olga Margalef Roberto Bao Sergi Pla-Rabes Blas Valero-Garcés Santiago Giralt

1 Botanic Institute of Barcelona (IBB-CSIC-ICUB), Barcelona, Spain 2 Department of Stratigraphy, Paleontology and Marine Sciences, Faculty of Geology, Universitat de Barcelona, Barcelona, Spain 3 Department of Geology, Faculty of Sciences, Universidade da Coruña, A Coruña, Spain 4 Center for Advanced Studies of Blanes (CEAB-CSIC), Blanes, Girona, Spain 5 Centre for Ecological Research and Fores...

2009
KAJ HOERNLE

Bacallado, J. J., G. Ortega, G. Delgado, and L. Moro. . La fauna de Canarias. Santa Cruz de Tenerife and Las Palmas de Gran Canaria, Canary Islands: Gobierno de Canarias, Consejería de Medio Ambiente y Ordenación Territorial, Centro de la Cultura Popular Canaria. Bramwell, D., and Z. Bramwell. . Wild fl owers of the Canary Islands, nd ed. Madrid: Editorial Rueda. Brito, A., P. J. Pascu...

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