Sardinia Coastal Uplift and Volcanism

Author(s):  
Patrizia Mariani ◽  
Carla Braitenberg ◽  
Fabrizio Antonioli
Keyword(s):  
2016 ◽  
Vol 31 (5) ◽  
pp. 376-387 ◽  
Author(s):  
Miklós Kázmér ◽  
Nilesh Bhatt ◽  
Vishal Ukey ◽  
Siddharth Prizomwala ◽  
Danko Taboroši ◽  
...  

2013 ◽  
Vol 14 (5) ◽  
pp. 1569-1589 ◽  
Author(s):  
Qian Yang ◽  
Shimon Wdowinski ◽  
Timothy H. Dixon

2016 ◽  
Vol 106 (1) ◽  
pp. 19-41 ◽  
Author(s):  
Christine Authemayou ◽  
Kevin Pedoja ◽  
Aicha Heddar ◽  
Stéphane Molliex ◽  
Azzedine Boudiaf ◽  
...  

1981 ◽  
Vol 46 (3) ◽  
pp. 619-626 ◽  
Author(s):  
Edwin N. Ferdon

Evidence indicates that several temporally distinct periods of prehistoric occupation of the now dry Santa Elena Peninsula of Ecuador coincided with periods of mangrove formation on the Peninsula. This article challenges the premise behind the hypothesis that such hydrophytic vegetation indicates greater rainfall during these periods. An alternative hypothesis is suggested, based upon the argument that known coastal uplift and probable accompanying physiographic changes first created, and later destroyed, the edaphic requirements for such a formation. The need to invoke a hypothesis of climatic shifts is thus dispensed with.


2010 ◽  
Vol 74 (2) ◽  
pp. 227-234 ◽  
Author(s):  
Toru Tamura ◽  
Fumitoshi Murakami ◽  
Kazuaki Watanabe

AbstractThis paper presents a case study that assessed spatial variations in the tectonic uplift rates of beach deposits in the relict Kujukuri strand plain, situated on the northeastern coast of the Boso Peninsula, eastern Japan. The southern Boso Peninsula is tilted downward to the northeast due to plate subduction along the Sagami Trough. However, the cause of the northeastern coast uplift creating the relict strand plain is unclear, due to the absence of a Holocene raised marine terrace sequence. Elevations and ages of beach deposits were collected from drilled cores and ground-penetrating radar profiles along three shore-normal sections in the southern Kujukuri strand plain. From this, alongshore variations in the relative sea level since the mid-Holocene could be seen. These corresponded to north-to-northeast downward tilting at a rate of 0.4 m/ka for an interval 10 km and are concordant with the longer term tilting of the last interglacial marine terrace surrounding the plain. Although it is difficult to assess shore-normal variations of uplift based on the present dataset, the recognized tilting apparently continues to the tilting of the southern Boso Peninsula, implying the Sagami Trough probably affects the uplift of the Kujukuri coast.


2010 ◽  
Vol 45 (1) ◽  
pp. 78-104 ◽  
Author(s):  
N. Palyvos ◽  
M. Mancini ◽  
D. Sorel ◽  
F. Lemeille ◽  
D. Pantosti ◽  
...  

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