نتایج جستجو برای: geochemistry

تعداد نتایج: 6460  

Journal: :pollution 2015
gholamabbas asadpour

evaluation of the geochemistry and hydrochemical quality of bam salt dome located in southern iran, was conducted in this study. two composite samples from salt units were collected and analysed by xrd and xrf to determine their mineral and elemental compositions. water samples were also collected from the only spring in the area and analysed for major anions, cations and some toxic elements. t...

Journal: :international journal of environmental research 2013
f.t. conceição g.r.b. navarro a.m. silva

the use of fertilizers npk and amendments in sugar cane crops may change the heavy metalsconcentrations in soils, making them available for plants and, consequently, they can be transferred to thehuman food chain. this study describes the redistribution of heavy metals (cd, cr, cu, ni, pb and zn) in soils with sugar cane crops due to fertilizers npk and amendments at corumbataí river basin, são...

2000
Ahren Bichler Peter T. Bobrowsky

During the 2000 field season, both regional and detailed till sampling surveys were conducted in the Cariboo region of central British Columbia (Figure 1). These surveys complement the longer term objectives of the NATMAP Ancient Pacific Margin (APM) project (see Nelson, 2000) and provide continuity to the surficial till geochemistry work initiated by Dixon-Warren and Hickin (2000) in 1999 as p...

2007

Exploration geochemistry continues to be a major contributor to mineral exploration programs at all scales. The decade has spanned a complete economic cycle in the minerals industry, during which there has been a change in exploration emphasis from the dominance of Au and diamonds to the addition of a range of base metals and the recent revival of U exploration. Increasing metal prices and the ...

2010
ROSEMARY LOUISE HICKEY

Boninites are unusual island arc volcanic rocks with high MgO (>9%), high Si0 2 (>55%) contents, and exceptionally low TiO 2 (<0.4%) contents. High MgO contents, MgO/(MgO + EFeO), Ni, Cr and Co contents indicate that boninites have equilibrated with mantle peridotite. Experimental petrologic studies and high Cr/(Cr + Al) in spinels in boninites suggest that they have separated from extremely re...

2006
T. Bose H. E. Newsom D. Sengupta

Introduction: The young Lonar crater, Maharashtra, India [1-3], is a bowl-shaped, almost circular, simple impact crater [4] of relatively small diameter ~1.8 km [5]. The uniqueness of this crater is that it is one of two known terrestrial impact craters excavated on basaltic target rock. The target-rock of this crater is the sub-horizontal Deccan basalt flows (~67 M.y.) [6]. All around the circ...

2014
Yong-Fei Zheng Joerg Hermann

The composition of continental subduction-zone fluids varies dramatically from dilute aqueous solutions at subsolidus conditions to hydrous silicate melts at supersolidus conditions, with variable concentrations of fluid-mobile incompatible trace elements. At ultrahigh-pressure (UHP) metamorphic conditions, supercritical fluids may occur with variable compositions. The water component of these ...

2014
G. Cowie H. Kitazato

Introduction Conclusions References

2007
KHAN M. G. MOSTOFA TAKAHITO YOSHIOKA EIICHI KONOHIRA EIICHIRO TANOUE

*Corresponding author (e-mail: [email protected]) *Present address: Field Science Education and Research Center, Kyoto University, Kitashirakawa, Oiwake, Kyoto 606-8502, Japan. **Present address: Institute of Geochemistry, The Chinese Academy of Sciences, 46 Guanshui Road, Guiyang/Guizhou 550002, China. †Present address: NPO Mori-no-za, Ina 396-0011, Japan. ‡Present address: Graduate ...

Journal: :Science 1979
I Steinhorn G Assaf J R Gat A Nishry A Nissenbaum M Stiller M Beyth D Neev R Garber G M Friedman W Weiss

Throttling of freshwater inputs into the meromictic Dead Sea weakened the long-term stability of the water column. Between 1975 and 1978 successive deepenings of the pycnocline from 70 meters to beyond 200 meters were recorded. Complete overturn finally took place during the winter of 1978-1979. This unique process was accompanied by changes in the geochemistry of several components.

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