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Raman Spectroscopy and X-Ray Diffraction Investigations of Phase Composition of Tiglit Meteorite. [PDF]
Materials (Basel)Karczemska A +4 more
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Microbially enhanced dissolution of calcite in sinking marine particles
Benedict Borer +4 more
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Deep microbial colonization during impact-generated hydrothermal circulation at the Lappajärvi impact structure, Finland. [PDF]
Nat CommunGustafsson J +9 more
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Ultrastructural changes in eggshell during incubation: mechanisms and implications. [PDF]
Poult SciRayan G, Fathi M.
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Science, 1963
Calcite-aragonite equilibrium, determined with an oscillating Griggs-Kennedy squeezer over the range 100° to 575°C, is given by P = 5500 (± 500) + 12.6 (± 1.5) T where pressure is in bars and temperature is in degrees Celsius.
G, Simmons, P, Bell
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Calcite-aragonite equilibrium, determined with an oscillating Griggs-Kennedy squeezer over the range 100° to 575°C, is given by P = 5500 (± 500) + 12.6 (± 1.5) T where pressure is in bars and temperature is in degrees Celsius.
G, Simmons, P, Bell
openaire +2 more sources
Application of EDTMPS as a novel calcite depressant in scheelite flotation
International Journal of Mining Science and Technology, 2023Congren Yang
exaly