Manganiferous minerals of the epidote group from the Archaean basement of West Greenland

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Standard

Manganiferous minerals of the epidote group from the Archaean basement of West Greenland. / Katerinopoulou, Anna; Balic Zunic, Tonci; Kolb, Jochen; Berger, Alfons; Secher, Karsten.

I: Bulletin of the Geological Society of Denmark, Bind 62, 2014, s. 27-37.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Katerinopoulou, A, Balic Zunic, T, Kolb, J, Berger, A & Secher, K 2014, 'Manganiferous minerals of the epidote group from the Archaean basement of West Greenland', Bulletin of the Geological Society of Denmark, bind 62, s. 27-37. <http://2dgf.dk/xpdf/bull62-27-37.pdf>

APA

Katerinopoulou, A., Balic Zunic, T., Kolb, J., Berger, A., & Secher, K. (2014). Manganiferous minerals of the epidote group from the Archaean basement of West Greenland. Bulletin of the Geological Society of Denmark, 62, 27-37. http://2dgf.dk/xpdf/bull62-27-37.pdf

Vancouver

Katerinopoulou A, Balic Zunic T, Kolb J, Berger A, Secher K. Manganiferous minerals of the epidote group from the Archaean basement of West Greenland. Bulletin of the Geological Society of Denmark. 2014;62:27-37.

Author

Katerinopoulou, Anna ; Balic Zunic, Tonci ; Kolb, Jochen ; Berger, Alfons ; Secher, Karsten. / Manganiferous minerals of the epidote group from the Archaean basement of West Greenland. I: Bulletin of the Geological Society of Denmark. 2014 ; Bind 62. s. 27-37.

Bibtex

@article{c543aec4db3e4d069b90a365cb7d4a50,
title = "Manganiferous minerals of the epidote group from the Archaean basement of West Greenland",
abstract = "The chemical compositions and crystal structures of Mn3+-containing minerals from the epidote group in Greenland rocks are investigated and described in detail. They occur in hydrothermally altered Archaean mafic sequences within the gneissic complex of the North Atlantic craton of West Greenland. The Mn-containing minerals have a characteristic red to pink colour. A detailed microchemical study shows a significant inter- and intra-sample variation in Mn content. The samples from different parageneses can be classified as Mn-bearing epidote and Mn-bearing clinozoisite. The intra-sample variation in the content of Al, Fe and Mn is on a very fine scale, but still allows for identification of a negative correlation between Mn and Fe. Textures indicate different stages of growth. Crystal chemical data are compared with literature data and illustrate the basic systematic differences between the influence of Fe and Mn on the crystal structure of the epidote group minerals.",
author = "Anna Katerinopoulou and {Balic Zunic}, Tonci and Jochen Kolb and Alfons Berger and Karsten Secher",
year = "2014",
language = "English",
volume = "62",
pages = "27--37",
journal = "Bulletin of the Geological Society of Denmark",
issn = "0011-6297",
publisher = "Dansk Geologisk Forening",

}

RIS

TY - JOUR

T1 - Manganiferous minerals of the epidote group from the Archaean basement of West Greenland

AU - Katerinopoulou, Anna

AU - Balic Zunic, Tonci

AU - Kolb, Jochen

AU - Berger, Alfons

AU - Secher, Karsten

PY - 2014

Y1 - 2014

N2 - The chemical compositions and crystal structures of Mn3+-containing minerals from the epidote group in Greenland rocks are investigated and described in detail. They occur in hydrothermally altered Archaean mafic sequences within the gneissic complex of the North Atlantic craton of West Greenland. The Mn-containing minerals have a characteristic red to pink colour. A detailed microchemical study shows a significant inter- and intra-sample variation in Mn content. The samples from different parageneses can be classified as Mn-bearing epidote and Mn-bearing clinozoisite. The intra-sample variation in the content of Al, Fe and Mn is on a very fine scale, but still allows for identification of a negative correlation between Mn and Fe. Textures indicate different stages of growth. Crystal chemical data are compared with literature data and illustrate the basic systematic differences between the influence of Fe and Mn on the crystal structure of the epidote group minerals.

AB - The chemical compositions and crystal structures of Mn3+-containing minerals from the epidote group in Greenland rocks are investigated and described in detail. They occur in hydrothermally altered Archaean mafic sequences within the gneissic complex of the North Atlantic craton of West Greenland. The Mn-containing minerals have a characteristic red to pink colour. A detailed microchemical study shows a significant inter- and intra-sample variation in Mn content. The samples from different parageneses can be classified as Mn-bearing epidote and Mn-bearing clinozoisite. The intra-sample variation in the content of Al, Fe and Mn is on a very fine scale, but still allows for identification of a negative correlation between Mn and Fe. Textures indicate different stages of growth. Crystal chemical data are compared with literature data and illustrate the basic systematic differences between the influence of Fe and Mn on the crystal structure of the epidote group minerals.

M3 - Journal article

VL - 62

SP - 27

EP - 37

JO - Bulletin of the Geological Society of Denmark

JF - Bulletin of the Geological Society of Denmark

SN - 0011-6297

ER -

ID: 152244575