نتایج جستجو برای: earth mantle

تعداد نتایج: 108664  

Journal: :Eos, Transactions American Geophysical Union 2002

Journal: :Geophysical Journal of the Royal Astronomical Society 2007

2015
D. A. Thompson J. O. S. Hammond

The mechanisms that drive the upwelling of chemical heterogeneity from the lower to upper mantle (e.g., thermal versus compositional buoyancy) are key to our understanding of whole mantle convective processes. We address these issues through a receiver function study on new seismic data from recent deployments located on the Afar Triple Junction, a location associated with deep mantle upwelling...

Journal: :Science 1979
A R Basu M Tatsumoto

The initial ratios of neodymium-143 to neodymium-144 in kimberlites ranging in age between 90 x 10(6) to 1300 x 10(6) years from South Africa, India, and the United States are different from the corresponding ratios in the minerals of peridotite inclusions in the kimberlites but are identical to the ratios in the basaltic achondrite Juvinas at the times of emplacement of the respective kimberli...

2007
Cin-Ty Aeolus Lee Qing-zhu Yin Adrian Lenardic Arnaud Agranier Craig J. O’Neill Nivedita Thiagarajan

New isotopic studies of Nd, the daughter product of the short-lived and now extinct isotope Sm, have revealed that the accessible part of the silicate Earth (e.g., upper mantle and crust) is more radiogenic in Nd/Nd than that of chondritic meteorites. The positive Nd anomaly of the Earth’s mantle implies that the Sm/Nd ratio of the mantle was fractionated early in Earth’s history and that the c...

2015
W. G. Ernst Norman H. Sleep Tatsuki Tsujimori

Intense devolatilization and chemical-density differentiation attended accretion of planetesimals on the primordial Earth. These processes gradually abated after cooling and solidification of an early magma ocean. By 4.3 or 4.2 Ga, water oceans were present, so surface temperatures had fallen far below lowpressure solidi of dry peridotite, basalt, and granite, ~1300, ~1120, and ~950 °C, respect...

2010
Satoru Yamamoto Ryosuke Nakamura Tsuneo Matsunaga Yoshiko Ogawa Yoshiaki Ishihara Tomokatsu Morota Naru Hirata Makiko Ohtake Takahiro Hiroi Yasuhiro Yokota Junichi Haruyama

The composition, structure and evolution of the Moon’s mantle is poorly constrained. The mineral olivine, one of the main constituents of Earth’s mantle, has been identified by Earth-based telescopic observations at two craters on the near side of the Moon, Aristarchus and Copernicus1–3. Global reflectance spectra in five discrete spectral bands produced by the spacecraft Clementine4–6 suggeste...

سعداله نصیری قیداری, , یوسفعلی عابدینی, ,

  we study the free oscillations of a non-rotating earth-like planet in the presence of a force free magnetic field. The model consists of a solid inner core, a liquid outer core and a solid mantle which is spherically symmetric. The lagrangian displacements are decomposed into scaloidal, poloidal and toroidal components using a gauged version of Helmholtz theorem. These components are identifi...

قاسمی, حبیب‎الله , کاظمی, زکیه ,

Outcrops of the Upper Ordovician igneous rocks, as basaltic lava and microgabbroic dyke and sill, present within the Abarsej and Ghelli formations in north and southwest of Shahrood. These rocks have basaltic, trachybasaltic and basaltic trachyandesitic composition with alkaline nature. Their parallel patterns on the primitive mantle and chondrite normalized spider diagrams indicate the common ...

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