Open AccessPalaeomagnetism of Pliocene‐Pleistocene sediments and lava flows on Tjörnes and Flatey, North Iceland
Author(s) -
EIRÍKSSON JÓN,
GUDMUNDSSON ANDRÉS I.,
KRISTJÁNSSON LEÓ,
GUNNARSSON KARL
Publication year - 1990
Publication title -
boreas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.95
H-Index - 74
eISSN - 1502-3885
pISSN - 0300-9483
DOI - 10.1111/j.1502-3885.1990.tb00420.x
Subject(s) - geology , paleontology , pleistocene , lava , paleomagnetism , stratigraphy , sedimentary rock , glacial period , sequence (biology) , volcano , tectonics , biology , genetics
Palaeomagnetic measurements have been carried out on lava flows and volcaniclastic sedimentary rocks of Upper Pliocene and Pleistocene age from sections on the Tjömes Peninsula and a core section from the island of Flatey off North Iceland. Earlier palaeomagnetic work in the area is reviewed, and new data on the stratigraphy of the Hoskuldsvik Group on Tjörnes are presented. A revised polarity column based on our resultsisset upfortheoutcropson Tjörnes, including twoadditionalnormalsubchronswithin the Matuyama. Our palaeomagnetic results indicate that the rocks penetrated by the Flatey drillhole accumulated during the Matuyama. Age estimates for the Upper Tjömes sequence are reviewed, and correlation alternatives indicate that the earliest glaciation of Tjörnes took place either at c.2 Ma or near the Gauss/Matuyama boundary at c. 2.5 Ma. Correlation of individual Matuyama subchrons remains uncertain. A comparison of the climatic evidence from the Tjörnes area with data on oxygen isotope and carbonate variations at DSDP site 552A is used to evaluate correlation alternatives.