First record of the Late Cretaceous denudation phase in the Admiralty Block (Transantarctic Mountains, northern Victoria Land, Antarctica)

被引：5

作者：

Balestrieri, ML

Bigazzi, G

机构：

[1] CNR, Ctr Studio Geol Appennino & Catene Perimediterran, I-50121 Florence, Italy

[2] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy

来源：

RADIATION MEASUREMENTS | 2001年 / 34卷 / 1-6期

关键词：

fission-track analysis; apatite; denudation; Transantarctic Mountains;

D O I：

10.1016/S1350-4487(01)00204-9

中图分类号：

TL [原子能技术]; O571 [原子核物理学];

学科分类号：

0827 ; 082701 ;

摘要：

Apatite fission-track analysis was performed on 13 granitoid samples of the Devonian Admiralty Intrusive Complex collected along two elevation profiles in the Admiralty Block, northern Victoria Land (NVL), East Antarctica. The sample age-elevation diagram shows a break in slope that indicates the presence of the Late Cretaceous phase of uplift and denudation already recognized in other sectors of NVL. Modeling of data suggests that the rocks may record also an Early Cenozoic pulse of denudation. (C) 2001 Elsevier Science Ltd. All rights reserved.

引用

页码：445 / 448

页数：4

共 11 条

[1]

Balestrieri M. L., 1997, ANTARCTIC REGION GEO, P547

[2] The Transantarctic Mountains: A natural laboratory for apatite fission-track analysis. Results from Italian Antarctic Expeditions [J].