Journal
GLOBAL AND PLANETARY CHANGE
Volume 24, Issue 3-4, Pages 261-274Publisher
ELSEVIER
DOI: 10.1016/S0921-8181(00)00012-6
Keywords
Mesozoic; Cenozoic; North East Greenland
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We present new apatite fission track data from SW Clavering O, East Greenland. The samples were collected from a vertical topographic profile covering similar to 1000 m of relief. The resulting data were modelled jointly to produce an internally consistent thermal history, reflecting denudationally induced shallow level crustal cooling since the Carboniferous. Three distinct events and a fourth less well-resolved event are inferred from the results of this new modelling approach. Maximum temperatures occurred in the Late Palaeozoic, implying a thicker Carboniferous sedimentary pile than presently observed. Early Jurassic cooling cannot be directly correlated to a well-documented period of elastic sedimentation in Hold-with-Hope, but may indicate sedimentation at this time in the Jurassic rift axis farther to the east. A later mid-Cretaceous cooling episode is reflected in the pre-Palaeogene basalt unconformity, and this denudation is likely to have shed large amounts of siliciclastic detritus into the proto-Voring Basin. Early Palaeogene burial occurred under a thick basaltic pile, and subsequently, denudation occurred during the Neogene to cool the rocks by similar to 50 degrees C, which may reflect 1-2 km of denudation. (C) 2000 Elsevier Science B.V. All rights reserved.
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