Geochemistry of Santorini tephra in lake sediments from Southwest Turkey

W. J. Eastwood; N. J. G. Pearce; J. A. Westgate; W. T. Perkins; H. F. Lamb; N. Roberts

doi:10.1016/S0921-8181(99)00005-3

Geochemistry of Santorini tephra in lake sediments from Southwest Turkey

W. J. Eastwood
, N. J. G. Pearce
, J. A. Westgate
, W. T. Perkins
, H. F. Lamb
, N. Roberts

Adran Daearyddiaeth a Gwyddorau Daear

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

88 Dyfyniadau (Scopus)

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A layer of volcanic ash (4 cm maximum recorded thickness) is present at ∼250 cm depth in littoral sediments of Gölhisar Gölü; a small intramontane lake in Southwest Turkey. The major-element glass chemistry, determined by electron microprobe, is characterised by a rhyolitic composition. Trace-element data, determined by solution inductively coupled plasma mass spectrometry (icp-ms) match previously reported results for proximal pumice samples from Santorini and Crete. Peat immediately below the tephra deposit has yielded radiocarbon ages of 3330±70 yr bp and 3225±45 yr bp (calibrated age range 1749–1406 bc).

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	17-29
Nifer y tudalennau	13
Cyfnodolyn	Global and Planetary Change
Cyfrol	21
Rhif cyhoeddi	1-3
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1016/S0921-8181(99)00005-3
Statws	Cyhoeddwyd - 01 Gorff 1999

Mynediad at Ddogfen

10.1016/S0921-8181(99)00005-3

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Dolen barhaus

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@article{183f70644922459195770102132f18fe,

title = "Geochemistry of Santorini tephra in lake sediments from Southwest Turkey",

abstract = "A layer of volcanic ash (4 cm maximum recorded thickness) is present at ∼250 cm depth in littoral sediments of G{\"o}lhisar G{\"o}l{\"u}; a small intramontane lake in Southwest Turkey. The major-element glass chemistry, determined by electron microprobe, is characterised by a rhyolitic composition. Trace-element data, determined by solution inductively coupled plasma mass spectrometry (icp-ms) match previously reported results for proximal pumice samples from Santorini and Crete. Peat immediately below the tephra deposit has yielded radiocarbon ages of 3330±70 yr bp and 3225±45 yr bp (calibrated age range 1749–1406 bc).",

keywords = "ICP-MS, Tephra, Tephrochronology, Trace-element geochemistry, Turkey",

author = "Eastwood, \{W. J.\} and Pearce, \{N. J. G.\} and Westgate, \{J. A.\} and Perkins, \{W. T.\} and Lamb, \{H. F.\} and N. Roberts",

note = "Funding Information: Fieldwork was funded in part by the National Geographic Society. WJE acknowledges the support of a University of Wales studentship. One of the radiocarbon dates was provided by NERC Scientific Services Radiocarbon Laboratory. Permission for our work was kindly granted by the General Directorate of Monuments and Museums, Burdur Province, Southwest Turkey. Thanks are also due to the British Institute of Archaeology at Ankara for the loan of the Dachnowsky corer.",

year = "1999",

month = jul,

day = "1",

doi = "10.1016/S0921-8181(99)00005-3",

language = "English",

volume = "21",

pages = "17--29",

journal = "Global and Planetary Change",

issn = "0921-8181",

publisher = "Elsevier",

number = "1-3",

}

TY - JOUR

T1 - Geochemistry of Santorini tephra in lake sediments from Southwest Turkey

AU - Eastwood, W. J.

AU - Pearce, N. J. G.

AU - Westgate, J. A.

AU - Perkins, W. T.

AU - Lamb, H. F.

AU - Roberts, N.

N1 - Funding Information: Fieldwork was funded in part by the National Geographic Society. WJE acknowledges the support of a University of Wales studentship. One of the radiocarbon dates was provided by NERC Scientific Services Radiocarbon Laboratory. Permission for our work was kindly granted by the General Directorate of Monuments and Museums, Burdur Province, Southwest Turkey. Thanks are also due to the British Institute of Archaeology at Ankara for the loan of the Dachnowsky corer.

PY - 1999/7/1

Y1 - 1999/7/1

N2 - A layer of volcanic ash (4 cm maximum recorded thickness) is present at ∼250 cm depth in littoral sediments of Gölhisar Gölü; a small intramontane lake in Southwest Turkey. The major-element glass chemistry, determined by electron microprobe, is characterised by a rhyolitic composition. Trace-element data, determined by solution inductively coupled plasma mass spectrometry (icp-ms) match previously reported results for proximal pumice samples from Santorini and Crete. Peat immediately below the tephra deposit has yielded radiocarbon ages of 3330±70 yr bp and 3225±45 yr bp (calibrated age range 1749–1406 bc).

AB - A layer of volcanic ash (4 cm maximum recorded thickness) is present at ∼250 cm depth in littoral sediments of Gölhisar Gölü; a small intramontane lake in Southwest Turkey. The major-element glass chemistry, determined by electron microprobe, is characterised by a rhyolitic composition. Trace-element data, determined by solution inductively coupled plasma mass spectrometry (icp-ms) match previously reported results for proximal pumice samples from Santorini and Crete. Peat immediately below the tephra deposit has yielded radiocarbon ages of 3330±70 yr bp and 3225±45 yr bp (calibrated age range 1749–1406 bc).

KW - ICP-MS

KW - Tephra

KW - Tephrochronology

KW - Trace-element geochemistry

KW - Turkey

UR - http://hdl.handle.net/2160/42741

UR - https://www.scopus.com/pages/publications/0032882067

U2 - 10.1016/S0921-8181(99)00005-3

DO - 10.1016/S0921-8181(99)00005-3

M3 - Article

SN - 0921-8181

VL - 21

SP - 17

EP - 29

JO - Global and Planetary Change

JF - Global and Planetary Change

IS - 1-3

ER -

Geochemistry of Santorini tephra in lake sediments from Southwest Turkey

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Mynediad at Ddogfen

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