Standard

Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan : an integrated methodology. / Khoury, Hani N.; Kokh, Svetlana N.; Sokol, Ella V. и др.

в: Arabian Journal of Geosciences, Том 9, № 6, 461, 01.05.2016.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Khoury, HN, Kokh, SN, Sokol, EV, Likhacheva, AY, Seryotkin, YV & Belogub, EV 2016, 'Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan: an integrated methodology', Arabian Journal of Geosciences, Том. 9, № 6, 461. https://doi.org/10.1007/s12517-016-2503-x

APA

Khoury, H. N., Kokh, S. N., Sokol, E. V., Likhacheva, A. Y., Seryotkin, Y. V., & Belogub, E. V. (2016). Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan: an integrated methodology. Arabian Journal of Geosciences, 9(6), [461]. https://doi.org/10.1007/s12517-016-2503-x

Vancouver

Khoury HN, Kokh SN, Sokol EV, Likhacheva AY, Seryotkin YV, Belogub EV. Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan: an integrated methodology. Arabian Journal of Geosciences. 2016 май 1;9(6):461. doi: 10.1007/s12517-016-2503-x

Author

Khoury, Hani N. ; Kokh, Svetlana N. ; Sokol, Ella V. и др. / Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan : an integrated methodology. в: Arabian Journal of Geosciences. 2016 ; Том 9, № 6.

BibTeX

@article{56baf939c25345d9a97aa9d71ab53929,
title = "Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan: an integrated methodology",
abstract = "Potentially new Ba–Sr phase with (Ca, Ba, Sr)10-x□x[(SO4)3(PO4)3](F−, O2−, Cl−)2 (1 < x < 2) composition belonging to the apatite supergroup was discovered in a recrystallized low-grade combustion metamorphic rocks of the Belqa Group, Central Jordan. The phase occurs as a fibrous subparallel aggregate and was originated by pseudomorphical replacement of precursor fish bone tissues embedded in biomicritic bituminous calcareous sediments. The mineralized fish bone was primarily composed of biogenic carbonate-fluorapatite. The Ba–Sr phase is monoclinic with space group P21/b, the unit cell parameters a = 18.881(19), b = 7.091(12), c = 8.951(12) {\AA}, β = 119.68(8)o, V = 1041.1(14) {\AA}3, and Z = 4. The empirical formula of the Ba–Sr phase is (Ca5.19Ba2.35Sr1.07Na0.06)Σ8.67[(S3.31P2.63Al0.03Si0.02V0.01)Σ6.00O24](F− 1.33O2− 0.58Cl− 0.01)Σ2.00. The primary textural heterogeneity of the bone tissues has controlled sharp compositional zonation of the Ba–Sr phase expressed in patchy distribution of Sr, Ba, Ca, P, and S. The newly-formed Ba–Sr phase represents the extreme case of interaction between precursor fossil biogenic carbonate-fluorapatite and associated Ba and Sr depot minerals (barite and celestine). The reaction took place during long-term and low-grade (T = 450–500 °C) combustion metamorphism of the calcareous sediments under dry conditions. The fossil bones were affected by drastic physical and chemical changes that were completed by the formation of a new mineral phase.",
keywords = "Apatite supergroup, Bituminous chalk, Central Jordan, Fossilization, Mineralized fish bone, Sr–Ba substitution, Trace elements",
author = "Khoury, {Hani N.} and Kokh, {Svetlana N.} and Sokol, {Ella V.} and Likhacheva, {Anna Yu} and Seryotkin, {Yurii V.} and Belogub, {Elena V.}",
year = "2016",
month = may,
day = "1",
doi = "10.1007/s12517-016-2503-x",
language = "English",
volume = "9",
journal = "Arabian Journal of Geosciences",
issn = "1866-7511",
publisher = "Springer-Verlag GmbH and Co. KG",
number = "6",

}

RIS

TY - JOUR

T1 - Ba and Sr mineralization of fossil fish bones from metamorphosed Belqa group sediments, Central Jordan

T2 - an integrated methodology

AU - Khoury, Hani N.

AU - Kokh, Svetlana N.

AU - Sokol, Ella V.

AU - Likhacheva, Anna Yu

AU - Seryotkin, Yurii V.

AU - Belogub, Elena V.

PY - 2016/5/1

Y1 - 2016/5/1

N2 - Potentially new Ba–Sr phase with (Ca, Ba, Sr)10-x□x[(SO4)3(PO4)3](F−, O2−, Cl−)2 (1 < x < 2) composition belonging to the apatite supergroup was discovered in a recrystallized low-grade combustion metamorphic rocks of the Belqa Group, Central Jordan. The phase occurs as a fibrous subparallel aggregate and was originated by pseudomorphical replacement of precursor fish bone tissues embedded in biomicritic bituminous calcareous sediments. The mineralized fish bone was primarily composed of biogenic carbonate-fluorapatite. The Ba–Sr phase is monoclinic with space group P21/b, the unit cell parameters a = 18.881(19), b = 7.091(12), c = 8.951(12) Å, β = 119.68(8)o, V = 1041.1(14) Å3, and Z = 4. The empirical formula of the Ba–Sr phase is (Ca5.19Ba2.35Sr1.07Na0.06)Σ8.67[(S3.31P2.63Al0.03Si0.02V0.01)Σ6.00O24](F− 1.33O2− 0.58Cl− 0.01)Σ2.00. The primary textural heterogeneity of the bone tissues has controlled sharp compositional zonation of the Ba–Sr phase expressed in patchy distribution of Sr, Ba, Ca, P, and S. The newly-formed Ba–Sr phase represents the extreme case of interaction between precursor fossil biogenic carbonate-fluorapatite and associated Ba and Sr depot minerals (barite and celestine). The reaction took place during long-term and low-grade (T = 450–500 °C) combustion metamorphism of the calcareous sediments under dry conditions. The fossil bones were affected by drastic physical and chemical changes that were completed by the formation of a new mineral phase.

AB - Potentially new Ba–Sr phase with (Ca, Ba, Sr)10-x□x[(SO4)3(PO4)3](F−, O2−, Cl−)2 (1 < x < 2) composition belonging to the apatite supergroup was discovered in a recrystallized low-grade combustion metamorphic rocks of the Belqa Group, Central Jordan. The phase occurs as a fibrous subparallel aggregate and was originated by pseudomorphical replacement of precursor fish bone tissues embedded in biomicritic bituminous calcareous sediments. The mineralized fish bone was primarily composed of biogenic carbonate-fluorapatite. The Ba–Sr phase is monoclinic with space group P21/b, the unit cell parameters a = 18.881(19), b = 7.091(12), c = 8.951(12) Å, β = 119.68(8)o, V = 1041.1(14) Å3, and Z = 4. The empirical formula of the Ba–Sr phase is (Ca5.19Ba2.35Sr1.07Na0.06)Σ8.67[(S3.31P2.63Al0.03Si0.02V0.01)Σ6.00O24](F− 1.33O2− 0.58Cl− 0.01)Σ2.00. The primary textural heterogeneity of the bone tissues has controlled sharp compositional zonation of the Ba–Sr phase expressed in patchy distribution of Sr, Ba, Ca, P, and S. The newly-formed Ba–Sr phase represents the extreme case of interaction between precursor fossil biogenic carbonate-fluorapatite and associated Ba and Sr depot minerals (barite and celestine). The reaction took place during long-term and low-grade (T = 450–500 °C) combustion metamorphism of the calcareous sediments under dry conditions. The fossil bones were affected by drastic physical and chemical changes that were completed by the formation of a new mineral phase.

KW - Apatite supergroup

KW - Bituminous chalk

KW - Central Jordan

KW - Fossilization

KW - Mineralized fish bone

KW - Sr–Ba substitution

KW - Trace elements

UR - http://www.scopus.com/inward/record.url?scp=84971619850&partnerID=8YFLogxK

U2 - 10.1007/s12517-016-2503-x

DO - 10.1007/s12517-016-2503-x

M3 - Article

AN - SCOPUS:84971619850

VL - 9

JO - Arabian Journal of Geosciences

JF - Arabian Journal of Geosciences

SN - 1866-7511

IS - 6

M1 - 461

ER -

ID: 25760757