scholarly journals Some Preliminary Results on the Early Holocene Shore Displacement in the Oskarshamn Area, South Eastern Sweden

1985 ◽  
Vol 35 (1) ◽  
pp. 119-134
Author(s):  
Nils-Olof Svensson

Abstract. In zwei 16 bzw. 26 m über Meeresspiegel gelegenen Seen sind Pollen- und Sedimentanalysen durchgeführt worden. Der Beginn der präborealen Chronozone ist hier durch eine Regression gekennzeichnet, die wahrscheinlich durch eine kurz dauernde Transgression unterbrochen gewesen ist. Eine rasche und recht bedeutsame Transgression, die mit der Ancylus-Transgression korreliert wird, setzte in beiden Lokalitäten um ca. 9000 v. h. ein. Zwischen ca. 9500 und 8500 v. h. wurden beide Seen vom Meer abgeschnürt, aber es ist bislang unbekannt, in welcher Höhenlage diese Regression ausgeklungen ist.

2002 ◽  
Vol 13 ◽  
pp. 1 ◽  
Author(s):  
Ian J. McNiven ◽  
Ian Thomas ◽  
Ugo Zoppi

<p>Coastal southeast Queensland is one of the most intensively studied archaeological regions of Australia. While the Fraser Island World Heritage Area is the most famous landscape in this coastal region, no archaeological excavations have been undertaken and its ancient Aboriginal past remains poorly understood. The Fraser Island Archaeological Project (FIAP) redresses this situation. Excavations at Waddy Point 1 Rockshelter (WP1) in July/August 2001 reveal a focus on local resources (shellfish, fish and tool stone) in the last c.900 years. This finding is consistent with McNiven's (1999) regionalisation model which posits marine resource intensification and the development of separate residential groups occupying the dune systems of Cooloola and Fraser Island in the last 1,000 years. Further excavation will be required to define the base of the cultural deposit of WP1, which may be early Holocene given arrival of the sea off the headland c.10,000 years ago.</p>


1978 ◽  
Vol 90 ◽  
pp. 67-73
Author(s):  
J Rose-Hansen ◽  
H Sørensen

In 1977 field work was concerned with the lujavrites and kakortokites of the south-eastern part of the Ilimaussaq alkaline intrusion (see Andersen & Bohse, this report), pegmatites and veins within the intrusion, the Narssaq intrusion situated to the west of the Ilimaussaq intrusion, and the environmental geochemistry and the ecology of the Narssaq region. Preliminary results of the field work and of some of the laboratory investigations are reported below. It should also be mentioned that a diamond drilling programme was carried out in the uraniferous rocks of the Kvanefjeld area in the northern part of the Ilimaussaq intrusion (see Nyegaard, this report).


2016 ◽  
Vol 10 (2) ◽  
pp. 369-388 ◽  
Author(s):  
Antonella Pedergnana ◽  
Andreu Ollé ◽  
Antony Borel ◽  
Marie-Hélène Moncel

2013 ◽  
Vol 28 (8) ◽  
pp. 777-788 ◽  
Author(s):  
YURENA YANES ◽  
MAGDALENA GÓMEZ‐PUCHE ◽  
MARCO A. ESQUEMBRE‐BEBIA ◽  
JAVIER FERNÁNDEZ‐LÓPEZ‐DE‐PABLO

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