As magnesium is enriched, a quadruple point with kainite exists.
2.
Caesium chloride occurs naturally as impurities in carnallite ( up to 0.002 % ), sylvite and kainite.
3.
Boracite is typically found in evaporite sequences associated with gypsum, anhydrite, halite, sylvite, carnallite, kainite and hilgardite.
4.
Carnallite occurs with a sequence of potassium and magnesium evaporite minerals : sylvite, kainite, picromerite, polyhalite, and kieserite.
5.
Kainite is a typical secondary mineral that forms through metamorphosis in marine deposits of potassium carbonate, and is also occasionally formed through resublimation from volcanic vapours.
6.
High levels of GHB have been shown to depress both the NMDA and AMPA / kainite receptor mediated functions and may also alter glutamatergic excitatory synaptic transmission as well.
7.
Kainite was discovered in the Stassfurt salt mines in today's Saxony-Anhalt, Germany in 1865 by the mine official Sch�ne and was first described by Carl Friedrich Jacob Zincken.
8.
The major ionotropic glutamine receptors include the N-methyl-D-aspartate ( NMDA ) and alpha-amino-3-hydroxy-5-methylisoxazole-4-propionic acid ( AMPA ) / kainite receptor.
9.
In salt ( NaCl ) saturated brine, leonite can be deposited from magnesium and potassium sulfate mixtures as low as 25 �C . The 25 �C isotherm of the system has leonite surrounded by sylvine, picromerite, astrakanite, epsomite, and kainite.
10.
"' Kainite "'( KMg ( SO 4 ) Cl?H 2 O ) is an evaporite mineral in the class of " Sulfates ( selenates, etc . ) with additional anions, with H 2 O " according to the Nickel-Strunz classification.
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