Matches in SemOpenAlex for { <https://semopenalex.org/work/W4382284212> ?p ?o ?g. }
- W4382284212 endingPage "1831" @default.
- W4382284212 startingPage "1810" @default.
- W4382284212 abstract "SUMMARY The Svecofennian gabbro intrusions coincide temporally with the global 2100–1800 Ma orogens related to the amalgamation of the Mesoproterozoic supercontinent Nuna. We provide a new reliable 1891–1875 Ma palaeomagnetic pole for Fennoscandia based on rock magnetic and palaeomagnetic studies on the Svecofennian intrusions in central Finland to fill gaps in the Palaeoproterozoic palaeomagnetic record. By using the new pole together with other global high-quality data, we propose a new palaeogeographic reconstruction at 1885 Ma. This, together with previous data, supports a long-lived relatively stable position of Fennoscandia at low to moderate latitudes at 1890–1790 Ma. Similar stable pole positions have also been obtained for Kalahari at 1880–1830 Ma, Siberia at 1880–1850 Ma, and possibly India at 1980–1775 Ma. A new reconstruction at the beginning of this period indicates the convergence of several cratons at 1885 Ma in the initial stages of the amalgamation of the Nuna supercontinent at low to moderate latitudes. The close proximity of cratons at low to moderate latitudes is further supported by global and regional palaeoclimatic indicators. Stable position of several cratons could indicate a global period of minimal apparent drift at ca. 1880–1830 Ma. Before this period, the global palaeomagnetic record indicates large back-and-forth swings, most prominently seen in the high-resolution 2020–1870 Ma Coronation loops of the Slave craton. These large back-and-forth movements have been explained as resulting from an unstable geomagnetic field or basin- or local-scale vertical-axis rotations. However, the most likely explanation is inertial interchange true polar wander (IITPW) events, which is in line with the suggestion of large amplitude true polar wander events during the formation of the supercontinent." @default.
- W4382284212 created "2023-06-28" @default.
- W4382284212 creator A5024848693 @default.
- W4382284212 creator A5027032709 @default.
- W4382284212 creator A5030378901 @default.
- W4382284212 creator A5043536668 @default.
- W4382284212 creator A5050045322 @default.
- W4382284212 date "2023-06-26" @default.
- W4382284212 modified "2023-09-27" @default.
- W4382284212 title "New palaeoproterozoic palaeomagnetic data from Central and Northern Finland indicate a long-lived stable position for Fennoscandia" @default.
- W4382284212 cites W1038600010 @default.
- W4382284212 cites W148089723 @default.
- W4382284212 cites W1622092127 @default.
- W4382284212 cites W1967350649 @default.
- W4382284212 cites W1967990603 @default.
- W4382284212 cites W1969447332 @default.
- W4382284212 cites W1979745670 @default.
- W4382284212 cites W1980328986 @default.
- W4382284212 cites W1980487623 @default.
- W4382284212 cites W1980655250 @default.
- W4382284212 cites W1984746465 @default.
- W4382284212 cites W1988309636 @default.
- W4382284212 cites W1991820195 @default.
- W4382284212 cites W1992565879 @default.
- W4382284212 cites W1992777544 @default.
- W4382284212 cites W1993856771 @default.
- W4382284212 cites W2002728547 @default.
- W4382284212 cites W2004686906 @default.
- W4382284212 cites W2007360474 @default.
- W4382284212 cites W2010462115 @default.
- W4382284212 cites W2011342565 @default.
- W4382284212 cites W2012432633 @default.
- W4382284212 cites W2016443673 @default.
- W4382284212 cites W2017176172 @default.
- W4382284212 cites W2018967433 @default.
- W4382284212 cites W2021154220 @default.
- W4382284212 cites W2023725435 @default.
- W4382284212 cites W2024634407 @default.
- W4382284212 cites W2025050632 @default.
- W4382284212 cites W2025569778 @default.
- W4382284212 cites W2027005472 @default.
- W4382284212 cites W2032852129 @default.
- W4382284212 cites W2032861618 @default.
- W4382284212 cites W2034833972 @default.
- W4382284212 cites W2034953607 @default.
- W4382284212 cites W2035674133 @default.
- W4382284212 cites W2036064397 @default.
- W4382284212 cites W2038045863 @default.
- W4382284212 cites W2038154149 @default.
- W4382284212 cites W2041824294 @default.
- W4382284212 cites W2041834782 @default.
- W4382284212 cites W2042118571 @default.
- W4382284212 cites W2042995040 @default.
- W4382284212 cites W2046268089 @default.
- W4382284212 cites W2047341001 @default.
- W4382284212 cites W2050402296 @default.
- W4382284212 cites W2056947557 @default.
- W4382284212 cites W2057770028 @default.
- W4382284212 cites W2060291004 @default.
- W4382284212 cites W2061712614 @default.
- W4382284212 cites W2064544769 @default.
- W4382284212 cites W2065742902 @default.
- W4382284212 cites W2068457255 @default.
- W4382284212 cites W2068595760 @default.
- W4382284212 cites W2069195241 @default.
- W4382284212 cites W2071561655 @default.
- W4382284212 cites W2073387347 @default.
- W4382284212 cites W2074332595 @default.
- W4382284212 cites W2075257616 @default.
- W4382284212 cites W2076214955 @default.
- W4382284212 cites W2079723891 @default.
- W4382284212 cites W2080502006 @default.
- W4382284212 cites W2083714035 @default.
- W4382284212 cites W2084312506 @default.
- W4382284212 cites W2088795933 @default.
- W4382284212 cites W2091755659 @default.
- W4382284212 cites W2095293118 @default.
- W4382284212 cites W2095800081 @default.
- W4382284212 cites W2096128075 @default.
- W4382284212 cites W2099717906 @default.
- W4382284212 cites W2101589526 @default.
- W4382284212 cites W2102521345 @default.
- W4382284212 cites W2105641585 @default.
- W4382284212 cites W2106142284 @default.
- W4382284212 cites W2114467958 @default.
- W4382284212 cites W2116153342 @default.
- W4382284212 cites W2117834512 @default.
- W4382284212 cites W2118204502 @default.
- W4382284212 cites W2118887933 @default.
- W4382284212 cites W2119025677 @default.
- W4382284212 cites W2121812998 @default.
- W4382284212 cites W2122112667 @default.
- W4382284212 cites W2128010703 @default.
- W4382284212 cites W2128556413 @default.
- W4382284212 cites W2140744246 @default.
- W4382284212 cites W2143817496 @default.
- W4382284212 cites W2151826977 @default.
- W4382284212 cites W2152666098 @default.