THERMOLUMINESCENCE DATING OF THE MIDDLE PLEISTOCENE RAISED BEACH OF SANGATTE (NORTHERN FRANCE)

被引：27

作者：

BALESCU, S

PACKMAN, SC

WINTLE, AG

GRUN, R

机构：

[1] UNIV CAMBRIDGE,DEPT GEOG,CAMBRIDGE CB2 3EN,ENGLAND

[2] UNIV COLL WALES,INST EARTH STUDIES,ABERYSTWYTH SY23 3DB,WALES

[3] UNIV CAMBRIDGE,SUBDEPT QUATERNARY RES,CAMBRIDGE CB2 3RS,ENGLAND

来源：

QUATERNARY RESEARCH | 1992年 / 37卷 / 03期

关键词：

D O I：

10.1016/0033-5894(92)90075-T

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

TL dating of both quartz and potassium feldspar grains from the Pleistocene beach of Sangatte, at the southern limit of the North Sea Basin, give self-consistent ages of 200,000 ± 45,000, 205,000 ± 14,000, and 229,000 ± 18,000 years, respectively. These results allow the beach deposits to be correlated with oxygen isotope stage 7 (244,000-190,000 yr) (Martinson et al., 1987). The existence of a fossil beach cliff line at 10 m above French O.D. demonstrates that the Strait of Dover was open during the penultimate interglaciation. © 1992.

引用

页码：390 / 396

页数：7

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