Reply: Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation

L A  Owen; L  Gualtieri; R C  Finkel; M W  Caffee; D I  Benn; M C  Sharma

doi:10.1002/jqs.680

Reply: Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation

L A Owen
, L Gualtieri
, R C Finkel
, M W Caffee
, D I Benn
, M C Sharma

Bell-Edwards Geographic Data Institute

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

Original language	English
Pages (from-to)	279-281
Number of pages	3
Journal	Journal of Quaternary Science
Volume	17
Issue number	3
DOIs	https://doi.org/10.1002/jqs.680
Publication status	Published - Mar 2002

Keywords

ASYNCHRONOUS GLACIATION
NANGA-PARBAT
PAKISTAN
MOUNTAINS

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Cite this

@article{d458bb13c07c41099a7032a46c17bd6d,

title = "Reply: Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation",

keywords = "ASYNCHRONOUS GLACIATION, NANGA-PARBAT, PAKISTAN, MOUNTAINS",

author = "Owen, \{L A\} and L Gualtieri and Finkel, \{R C\} and Caffee, \{M W\} and Benn, \{D I\} and Sharma, \{M C\}",

year = "2002",

month = mar,

doi = "10.1002/jqs.680",

language = "English",

volume = "17",

pages = "279--281",

journal = "Journal of Quaternary Science",

issn = "0267-8179",

publisher = "John Wiley \& Sons, Ltd",

number = "3",

}

TY - JOUR

T1 - Reply: Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation

AU - Owen, L A

AU - Gualtieri, L

AU - Finkel, R C

AU - Caffee, M W

AU - Benn, D I

AU - Sharma, M C

PY - 2002/3

Y1 - 2002/3

KW - ASYNCHRONOUS GLACIATION

KW - NANGA-PARBAT

KW - PAKISTAN

KW - MOUNTAINS

U2 - 10.1002/jqs.680

DO - 10.1002/jqs.680

M3 - Letter

SN - 0267-8179

VL - 17

SP - 279

EP - 281

JO - Journal of Quaternary Science

JF - Journal of Quaternary Science

IS - 3

ER -