2001
DOI: 10.1016/s0925-8388(01)01613-9
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Synthesis and characterization of Fe–Cl boracite

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Cited by 2 publications
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“…These are thought to be the result of transition from an unstable high temperature isometric form upon cooling. The mineral is related to the homonymous group that includes chambersite -(Mn 2+ ) 3 B 7 O 13 Cl, congolite -(Fe 2+ , Mg) 3 B 7 O 13 Cl, ericaite -(Fe 2+ ) 3 B 7 O 13 Cl and, trembathite -(Mg, Fe 2+ ) 3 B 7 O 13 Cl (Burns and Carpenter [26]). Boracite is typically found in evaporite sequences associated with gypsum, anhydrite, halite, sylvite, carnallite, kainite and hilgardite.…”
Section: Introductionmentioning
confidence: 99%
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“…These are thought to be the result of transition from an unstable high temperature isometric form upon cooling. The mineral is related to the homonymous group that includes chambersite -(Mn 2+ ) 3 B 7 O 13 Cl, congolite -(Fe 2+ , Mg) 3 B 7 O 13 Cl, ericaite -(Fe 2+ ) 3 B 7 O 13 Cl and, trembathite -(Mg, Fe 2+ ) 3 B 7 O 13 Cl (Burns and Carpenter [26]). Boracite is typically found in evaporite sequences associated with gypsum, anhydrite, halite, sylvite, carnallite, kainite and hilgardite.…”
Section: Introductionmentioning
confidence: 99%
“…Vibrational spectroscopy has focussed on the ferroelectric transitions [17][18][19][20][21][22][23][24]. Different types of boracites have been synthesised [25][26][27].…”
Section: Introductionmentioning
confidence: 99%