NDLI: The Mesoproterozoic basement in the southern Baltic Sea: insights from the G 14

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The Mesoproterozoic basement in the southern Baltic Sea: insights from the G 14–1 off-shore borehole

Content Provider	Springer Nature Link
Author	Obst, Karsten Hammer, Jörg Katzung, Gerhard Korich, Dietmar
Copyright Year	2004
Abstract	The continuation of the Mesoproterozoic basement of the southern Fennoscandian Shield is documented in the G 14–1 off-shore borehole, northeast of the island of Rügen, where crystalline rocks of monzogranitic composition occur beneath flat-lying early Palaeozoic sediments at a depth of approximately 2,000 m. The greenish-grey, or partly reddish-grey, granites show a slightly porphyritic texture marked by plagioclase crystals or aggregates in a groundmass dominated by fresh microcline. Chloritized biotite occurs as a subordinate mafic phase. Ductile and brittle deformation is indicated by a weak foliation and the occurrence of several cataclastic zones, respectively. Major and trace element geochemistry suggest that these rocks are K-rich calc-alkaline granites and represent a restite-poor melting product of a granodioritic protolith. The low MgO, Cr, Ni and Co concentrations and relatively high content of accessory phases (apatite, zircon) point to formation of water undersaturated, high temperature (>900 °C) melts at low degrees of partial melting. Although the G 14 granite lacks hornblende, in contrast to most of the granites from Bornholm, it seems geochemically related to them. Analysed samples mostly fit an intermediate position between the Rønne and Vang granitoids, which both belong to a group of Mesoproterozoic intrusions showing partial ductile deformation. (Y+Nb) vs. Rb plots suggest that all these granitic rocks were generated in intracratonic conditions. A genetic relationship between them and contemporaneously intruded Karlshamn-group granites in Blekinge, eastern Scania and Småland is supported by intrusion age of 1,460±3 Ma obtained from Pb-Pb isotope ratios measured on single zircons of the G 14 granite.
Starting Page	1
Ending Page	12
Page Count	12
File Format	PDF
ISSN	14373254
Journal	International Journal of Earth Sciences
Volume Number	93
Issue Number	1
e-ISSN	14373262
Language	English
Publisher	Springer-Verlag
Publisher Date	2004-01-22
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Blekinge-Bornholm Danopolonian Orogeny Fennoscandian Shield G 14 granite Mesoproterozoic crust NE Germany Pb-Pb zircon ages
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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