Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC

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

Standard

Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC. / Makovicky, Emil; Parisatto, Matteo; Højlund, Flemming.

In: Archaeometry, Vol. 57, No. 1, 02.2015, p. 163-176.

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

Harvard

Makovicky, E, Parisatto, M & Højlund, F 2015, 'Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC', Archaeometry, vol. 57, no. 1, pp. 163-176. https://doi.org/10.1111/arcm.12088

APA

Makovicky, E., Parisatto, M., & Højlund, F. (2015). Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC. Archaeometry, 57(1), 163-176. https://doi.org/10.1111/arcm.12088

Vancouver

Makovicky E, Parisatto M, Højlund F. Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC. Archaeometry. 2015 Feb;57(1):163-176. https://doi.org/10.1111/arcm.12088

Author

Makovicky, Emil ; Parisatto, Matteo ; Højlund, Flemming. / Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC. In: Archaeometry. 2015 ; Vol. 57, No. 1. pp. 163-176.

Bibtex

@article{6245e2ad2a07498bb8f64a715d6d906d,
title = "Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC",
abstract = "A scalenohedral hematite pendant (presumably a pseudomorph after a calcite crystal), excavated on Bahrain (ancient Dilmun) in the Persian Gulf from layers dated to c.1800 bc, was investigated using X-ray computed microtomography. The internal porosity was studied in 3D, showing a preferential concentration of small pores in the central part, where carbonate remnants might still be present, and larger, flattened, elongated voids in the subsurface portion. Part of the scalenohedron can be described as an intergrowth of platy hematite crystals. Microtomography also yielded data on pore-size distribution. Considerations are given to the genetic model and the provenance of the hematite pendant.",
author = "Emil Makovicky and Matteo Parisatto and Flemming H{\o}jlund",
year = "2015",
month = feb,
doi = "10.1111/arcm.12088",
language = "English",
volume = "57",
pages = "163--176",
journal = "Archaeometry",
issn = "0003-813X",
publisher = "Wiley-Blackwell",
number = "1",

}

RIS

TY - JOUR

T1 - Non-Destructive investigation of a scalenohedral hematite pendant from Bahrain, c. 1800 BC

AU - Makovicky, Emil

AU - Parisatto, Matteo

AU - Højlund, Flemming

PY - 2015/2

Y1 - 2015/2

N2 - A scalenohedral hematite pendant (presumably a pseudomorph after a calcite crystal), excavated on Bahrain (ancient Dilmun) in the Persian Gulf from layers dated to c.1800 bc, was investigated using X-ray computed microtomography. The internal porosity was studied in 3D, showing a preferential concentration of small pores in the central part, where carbonate remnants might still be present, and larger, flattened, elongated voids in the subsurface portion. Part of the scalenohedron can be described as an intergrowth of platy hematite crystals. Microtomography also yielded data on pore-size distribution. Considerations are given to the genetic model and the provenance of the hematite pendant.

AB - A scalenohedral hematite pendant (presumably a pseudomorph after a calcite crystal), excavated on Bahrain (ancient Dilmun) in the Persian Gulf from layers dated to c.1800 bc, was investigated using X-ray computed microtomography. The internal porosity was studied in 3D, showing a preferential concentration of small pores in the central part, where carbonate remnants might still be present, and larger, flattened, elongated voids in the subsurface portion. Part of the scalenohedron can be described as an intergrowth of platy hematite crystals. Microtomography also yielded data on pore-size distribution. Considerations are given to the genetic model and the provenance of the hematite pendant.

U2 - 10.1111/arcm.12088

DO - 10.1111/arcm.12088

M3 - Journal article

VL - 57

SP - 163

EP - 176

JO - Archaeometry

JF - Archaeometry

SN - 0003-813X

IS - 1

ER -

ID: 99344297