Order–disorder–reorder process in thermally treated dolomite samples: a combined powder and single-crystal X-ray diffraction study

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Order–disorder–reorder process in thermally treated dolomite samples : a combined powder and single-crystal X-ray diffraction study. / Zucchini, Azzurra; Comodi, Paola; Katerinopoulou, Anna; Balic Zunic, Tonci; McCammon, Cathrin; Frondini, F.

In: Physics and Chemistry of Minerals, Vol. 39, No. 4, 2012, p. 319–328.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Zucchini, A, Comodi, P, Katerinopoulou, A, Balic Zunic, T, McCammon, C & Frondini, F 2012, 'Order–disorder–reorder process in thermally treated dolomite samples: a combined powder and single-crystal X-ray diffraction study', Physics and Chemistry of Minerals, vol. 39, no. 4, pp. 319–328. https://doi.org/10.1007/s00269-012-0489-9

APA

Zucchini, A., Comodi, P., Katerinopoulou, A., Balic Zunic, T., McCammon, C., & Frondini, F. (2012). Order–disorder–reorder process in thermally treated dolomite samples: a combined powder and single-crystal X-ray diffraction study. Physics and Chemistry of Minerals, 39(4), 319–328. https://doi.org/10.1007/s00269-012-0489-9

Vancouver

Zucchini A, Comodi P, Katerinopoulou A, Balic Zunic T, McCammon C, Frondini F. Order–disorder–reorder process in thermally treated dolomite samples: a combined powder and single-crystal X-ray diffraction study. Physics and Chemistry of Minerals. 2012;39(4):319–328. https://doi.org/10.1007/s00269-012-0489-9

Author

Zucchini, Azzurra ; Comodi, Paola ; Katerinopoulou, Anna ; Balic Zunic, Tonci ; McCammon, Cathrin ; Frondini, F. / Order–disorder–reorder process in thermally treated dolomite samples : a combined powder and single-crystal X-ray diffraction study. In: Physics and Chemistry of Minerals. 2012 ; Vol. 39, No. 4. pp. 319–328.

Bibtex

@article{ccf408af6cd84157af5cc517069d1c51,
title = "Order–disorder–reorder process in thermally treated dolomite samples: a combined powder and single-crystal X-ray diffraction study",
abstract = "A combined powder and single-crystal X-ray diffraction analysis of dolomite [CaMg(CO3)2] heated to 1,200oC at 3 GPa was made to study the order–disorder–reorder process. The order/disorder transition is inferred to start below 1,100oC, and complete disorder is attained at approximately 1,200oC. Twinned crystals characterized by high internal order were found in samples annealed over 1,100oC, and their fraction was found to increase with temperature. Evidences of twinning domains combined with probable remaining disordered portions of the structure imply that reordering processes occur during the quench. Twin domains are hereby proposed as a witness to thermally induced intra-layer-type cation disordering.",
author = "Azzurra Zucchini and Paola Comodi and Anna Katerinopoulou and {Balic Zunic}, Tonci and Cathrin McCammon and F. Frondini",
year = "2012",
doi = "10.1007/s00269-012-0489-9",
language = "English",
volume = "39",
pages = "319–328",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer",
number = "4",

}

RIS

TY - JOUR

T1 - Order–disorder–reorder process in thermally treated dolomite samples

T2 - a combined powder and single-crystal X-ray diffraction study

AU - Zucchini, Azzurra

AU - Comodi, Paola

AU - Katerinopoulou, Anna

AU - Balic Zunic, Tonci

AU - McCammon, Cathrin

AU - Frondini, F.

PY - 2012

Y1 - 2012

N2 - A combined powder and single-crystal X-ray diffraction analysis of dolomite [CaMg(CO3)2] heated to 1,200oC at 3 GPa was made to study the order–disorder–reorder process. The order/disorder transition is inferred to start below 1,100oC, and complete disorder is attained at approximately 1,200oC. Twinned crystals characterized by high internal order were found in samples annealed over 1,100oC, and their fraction was found to increase with temperature. Evidences of twinning domains combined with probable remaining disordered portions of the structure imply that reordering processes occur during the quench. Twin domains are hereby proposed as a witness to thermally induced intra-layer-type cation disordering.

AB - A combined powder and single-crystal X-ray diffraction analysis of dolomite [CaMg(CO3)2] heated to 1,200oC at 3 GPa was made to study the order–disorder–reorder process. The order/disorder transition is inferred to start below 1,100oC, and complete disorder is attained at approximately 1,200oC. Twinned crystals characterized by high internal order were found in samples annealed over 1,100oC, and their fraction was found to increase with temperature. Evidences of twinning domains combined with probable remaining disordered portions of the structure imply that reordering processes occur during the quench. Twin domains are hereby proposed as a witness to thermally induced intra-layer-type cation disordering.

U2 - 10.1007/s00269-012-0489-9

DO - 10.1007/s00269-012-0489-9

M3 - Journal article

VL - 39

SP - 319

EP - 328

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

SN - 0342-1791

IS - 4

ER -

ID: 49378177