Magnesium rock, distribution

Worldwide distribution of magnesium-rich ultramafic rocks. 

Saxena S. K. (1968). Distribution of iron and magnesium between coexisting garnet and clino-pyroxene in rocks of varying metamorphic grade. Amer. Mineral, 53 2018-2021. 

The dominance of carbonate hydrolysis, carbo-nation, and sulfide oxidation in subglacial weathering reactions on aluminosilicate/silicate bedrock is also found on carbonate bedrock. However, the balance between carbonate dissolution and sulfide oxidation depends on the spatial distribution of sulfides in the bedrock and basal debris (Fairchild et al., 1999). Noncongruent dissolution of strontium and magnesium from carbonate is also observed in high rock water weathering environments, such as the distributed drainage systems, in which water flow is also low (Fairchild et al., 1999). 

Fig. 3 Worldwide distribution of magnesium-rich ultramafic rocks. (From Ref " 1) (View this art in color at www.dekker.com.)...

Figure 3 The distribution of neon isotopes in mantle-derived rocks, indicating the presence of an atmospheric component, a radiogenic component adding Ne (produced by neutrons from uranium fission acting on oxygen and magnesium), and a solar component. It is this latter that indicates that gases in the mantle were derived from the capture of solar material in the early history of the Earth. M = MORB (midocean ridge basalts) P = plume or ocean island basalts (OIB) A = atmosphere. Solar neon is represented by the horizontal line at Ne/ Ne = 12.5 MFL is the mass fractionation line. The presence of solar neon in ocean basalts was first identified by Craig and Lupton (Craig H and Lupton JE (1976) Earth and Planetary Science Letters 31 369-385). (Reprinted with permission from Farley and Poreda (1993).

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