Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams. / Yorke, L.; Rumsby, B.T.; Chiverrell, R.C.
Yn: Proceedings of the Geologists' Association, Cyfrol 123, Rhif 4, 01.08.2012, t. 608-625.

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

HarvardHarvard

Yorke, L, Rumsby, BT & Chiverrell, RC 2012, 'Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams', Proceedings of the Geologists' Association, cyfrol. 123, rhif 4, tt. 608-625. https://doi.org/10.1016/j.pgeola.2012.03.005

APA

Yorke, L., Rumsby, B. T., & Chiverrell, R. C. (2012). Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams. Proceedings of the Geologists' Association, 123(4), 608-625. https://doi.org/10.1016/j.pgeola.2012.03.005

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MLA

VancouverVancouver

Yorke L, Rumsby BT, Chiverrell RC. Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams. Proceedings of the Geologists' Association. 2012 Awst 1;123(4):608-625. doi: 10.1016/j.pgeola.2012.03.005

Author

Yorke, L. ; Rumsby, B.T. ; Chiverrell, R.C. / Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams. Yn: Proceedings of the Geologists' Association. 2012 ; Cyfrol 123, Rhif 4. tt. 608-625.

RIS

TY - JOUR

T1 - Depositional history of the Tyne valley associated with retreat and stagnation of Late Devensian Ice Streams

AU - Yorke, L.

AU - Rumsby, B.T.

AU - Chiverrell, R.C.

PY - 2012/8/1

Y1 - 2012/8/1

U2 - 10.1016/j.pgeola.2012.03.005

DO - 10.1016/j.pgeola.2012.03.005

M3 - Article

VL - 123

SP - 608

EP - 625

JO - Proceedings of the Geologists' Association

JF - Proceedings of the Geologists' Association

SN - 0016-7878

IS - 4

ER -