Coarse-grained terrigenous sediment deposition on continental rise drifts: A record of Plio-Pleistocene glaciation on the Antarctic Peninsula

Ellen A. Cowan; Claus-Dieter Hillenbrand; Lauren E. Hassler; Matthew T. Ake

doi:10.1016/j.palaeo.2008.03.010

Coarse-grained terrigenous sediment deposition on continental rise drifts: A record of Plio-Pleistocene glaciation on the Antarctic Peninsula

Ellen A. Cowan
, Claus-Dieter Hillenbrand
, Lauren E. Hassler
, Matthew T. Ake

Appalachian State University

British Antarctic Survey
Appalachian State University

Research output: Contribution to journal › Article › peer-review

Original language	American English
Journal	Palaeogeography, Palaeoclimatology, Palaeoecology
Volume	265
DOIs	https://doi.org/10.1016/j.palaeo.2008.03.010
State	Published - Aug 1 2008

Disciplines

Geology
Geomorphology
Paleontology

Access to Document

10.1016/j.palaeo.2008.03.010License: Unspecified

Cite this

@article{fefe5274481a45918f9e16e77e8d23be,

title = "Coarse-grained terrigenous sediment deposition on continental rise drifts: A record of Plio-Pleistocene glaciation on the Antarctic Peninsula",

author = "Cowan, \{Ellen A.\} and Claus-Dieter Hillenbrand and Hassler, \{Lauren E.\} and Ake, \{Matthew T.\}",

note = "JavaScript is disabled on your browser. Please enable JavaScript to use all the features on this page. Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y.",

year = "2008",

month = aug,

day = "1",

doi = "10.1016/j.palaeo.2008.03.010",

language = "American English",

volume = "265",

journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",

}

TY - JOUR

T1 - Coarse-grained terrigenous sediment deposition on continental rise drifts: A record of Plio-Pleistocene glaciation on the Antarctic Peninsula

AU - Cowan, Ellen A.

AU - Hillenbrand, Claus-Dieter

AU - Hassler, Lauren E.

AU - Ake, Matthew T.

N1 - JavaScript is disabled on your browser. Please enable JavaScript to use all the features on this page. Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y.

PY - 2008/8/1

Y1 - 2008/8/1

UR - https://www.sciencedirect.com/science/article/pii/S0031018208001922

U2 - 10.1016/j.palaeo.2008.03.010

DO - 10.1016/j.palaeo.2008.03.010

M3 - Article

VL - 265

JO - Palaeogeography, Palaeoclimatology, Palaeoecology

JF - Palaeogeography, Palaeoclimatology, Palaeoecology

ER -