Thermal history solutions from thermochronology must be governed by geological relationships: A comment on Jess et al. (2019)

被引：5
|
作者：
Green, Paul F. [1 ]
Japsen, Peter [2 ]
Bonow, Johan M. [3 ,4 ]
Chalmers, James A. [2 ]
Duddy, Ian R. [1 ]
机构：
[1] Geotrack Int, 37 Melville Rd, Brunswick West, Vic 3055, Australia
[2] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen, Denmark
[3] Geovisiona AB, SE-19792 Bro, Sweden
[4] Uppsala Univ, SE-75105 Uppsala, Sweden
来源：
GEOMORPHOLOGY | 2020年 / 360卷
关键词：
PASSIVE CONTINENTAL MARGINS; CENTRAL WEST GREENLAND; GLACIAL EROSION; NUUSSUAQ BASIN; APATITE (U-TH)/HE; UPLIFT; EVOLUTION; DATASETS;
D O I：
10.1016/j.geomorph.2019.106848
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
The recent study of the basement margin to the Nuussuaq Basin, West Greenland, by Jess et al. (2019) illustrates the problems introduced by extracting thermal histories from thermochronology data without taking into account the constraints provided by geological evidence. Their interpretations are incompatible with numerous aspects of the geology of the region, and as a result their conclusions are not valid. (C) 2019 Elsevier B.V. All rights reserved.
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页数：3
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