1 – 12 of 12
- show: 20
- |
- sort: year (new to old)
Close
Embed this list
<iframe src=" "
width=" "
height=" "
allowtransparency="true"
frameborder="0">
</iframe>
- 2024
-
Mark
Exploring the potential of rock surface luminescence from glacial sediments : dating and transport history
2024) In Boreas(
- Contribution to journal › Article
- 2019
-
Mark
Luminescence rock surface profiles from moraine boulders: useful for dating and transport histories
2019) EGU General Assembly(
- Contribution to conference › Abstract
-
Mark
Glacial history and palaeo-environmental change of southern Taimyr Peninsula, Arctic Russia, during the Middle and Late Pleistocene
(
- Contribution to journal › Article
-
Mark
Data set on sedimentology, palaeoecology and chronology of Middle to Late Pleistocene deposits on the Taimyr Peninsula, Arctic Russia
(
- Contribution to journal › Article
- 2016
-
Mark
The north-eastern aeolian 'European Sand Belt' as potential record of environmental changes : A case study from Eastern Latvia and Southern Estonia
(
- Contribution to journal › Article
- 2015
-
Mark
Age and sedimentary record of inland eolian sediments in Lithuania, NE European Sand Belt
(
- Contribution to journal › Article
- 2013
-
Mark
An interglacial polar bear and an early Weichselian glaciation at Poolepynten, western Svalbard
(
- Contribution to journal › Article
- 2012
-
Mark
Luminescence signals from modern sediments in a glaciated bay, NW Svalbard
(
- Contribution to journal › Article
- 2011
-
Mark
A multi-method approach to dating middle and late Quaternary high relative sea-level events on NW Svalbard - A case study
(
- Contribution to journal › Article
- 2010
-
Mark
Re-dating the Pilgrimstad Interstadial with OSL: a warmer climate and a smaller ice sheet during the Swedish Middle Weichselian (MIS 3)?
(
- Contribution to journal › Article
- 2009
-
Mark
Late Quaternary ice sheet, lake and sea history of southwest Scandinavia - a synthesis
(
- Contribution to journal › Scientific review
- 2007
-
Mark
Was southern Sweden ice free at 19-25 ka, or were the post LGM glacifluvial sediments incompletely bleached?
(
- Contribution to journal › Article