Reference Type | Journal (article/letter/editorial) |
---|
Access Rights | Open Access |
---|
Title | Sm-Nd and Rb-Sr ages of hornblende clinopyroxenite and metagabbro from the Lillebukt Alkaline Complex,Seiland Igneous Province |
---|
Journal | Norsk Geologisk Tidsskrift [Norwegian Journal of Geology] | ISBN | 0029-196X |
---|
Authors | Cadow, Renate | Author |
---|
Year | 1993 | Volume | 73 |
---|
Page(s) | 243-249 | Issue | 4 |
---|
Publisher | Geological Society of Norway |
---|
Download URL | https://njg.geologi.no/images/NJG_articles/NGT_73_4_243-249.pdf+ |
---|
Classification | Not set | LoC | Not set |
---|
Mindat Ref. ID | 16512557 | Long-form Identifier | mindat:1:5:16512557:4 |
---|
|
GUID | 647da164-5604-4a82-a41d-137cd6536ee8 |
---|
Full Reference | Cadow, Renate (1993) Sm-Nd and Rb-Sr ages of hornblende clinopyroxenite and metagabbro from the Lillebukt Alkaline Complex,Seiland Igneous Province. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 73 (4) 243-249 |
---|
Plain Text | Cadow, Renate (1993) Sm-Nd and Rb-Sr ages of hornblende clinopyroxenite and metagabbro from the Lillebukt Alkaline Complex,Seiland Igneous Province. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 73 (4) 243-249 |
---|
In | (1993) Norsk Geologisk Tidsskrift [Norwegian Journal of Geology] Vol. 73 (4) Geological Society of Norway |
---|
Abstract/Notes | Apatite-rich hornblende clinopyroxenite from the Lillebukt Alkaline Complex, Stjernøy, has yielded Sm-Nd and Rb-Sr internal isochron ages of 540 ± 39 Ma (MSWD = 0.21) and 521 ± 22 Ma (MSWD = 0.00) respectively, interpreted as intrusion ages. ?NdtCHUR of +4.00 ± 0.55 and ?SrtUR of -11.21 ± 0.34 suggest a moderately depleted mantle source. The metagabbro host, which was deformed before emplacement of the horn blende pyroxenite dykes, gives Sm-Nd and Rb-Sr internal isochron ages of 517 ± 61 Ma (MSWD = 1.64) and 534 ± 8 Ma (MSWD = 4.60) respectively. Both probably date metamorphic recrystallization of the host metagabbro that took place before the initiation of the alkaline magmatism. |
---|
These are possibly similar items as determined by title/reference text matching only.