1-7 OF 7 RESULTS FOR

Chara-Sinsk dike swarm

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 October 2002
Russ. Geol. Geophys. (2002) 43 (10): 916–927.
... that monzonitoids of different types of occurrence have in general similar chemical composition and the PMIC rocks are very close to quartz syenite-porphyries of composite dikes of the Chara-Sinsk Dike Swarm (CSDS). Similarity between the geodynamic settings of intrusions from the CSDS (Vilyui Paleorift System...
FIGURES | View All (7)
Journal Article
Published: 01 October 2018
Russ. Geol. Geophys. (2018) 59 (10): 1204–1216.
... and subalkaline varieties. The basites of the CharaSinsk swarm occurs as a few dikes of common tholeiites. However, most of the intrusions are represented by high-alkaline melts, and based on their major element compositions, they fall into the field of subalkaline dolerites. The Middle Paleozoic Vilyui...
FIGURES | View All (7)
Image
Geochemical diagrams for dolerites dated in this study.  а  –  TAS diagram ...
Published: 01 July 2024
et al., 2020 ); 2 – dikes of the YVLIP from ( Polyansky et al., 2017 ); 3 – basic rocks of the Vilyui–Markha swarm from ( Kiselev et al., 2012 ); 4 – basalt and dolerite from individual complexes: Vilyui–Markha (mean for 4 samples), CharaSinsk (mean for 5 samples), Dyakhtar ( Masaitis, 2006 ).
Journal Article
Published: 01 July 2024
Russ. Geol. Geophys. (2024) 65 (7): 814–830.
... et al., 2020 ); 2 – dikes of the YVLIP from ( Polyansky et al., 2017 ); 3 – basic rocks of the Vilyui–Markha swarm from ( Kiselev et al., 2012 ); 4 – basalt and dolerite from individual complexes: Vilyui–Markha (mean for 4 samples), CharaSinsk (mean for 5 samples), Dyakhtar ( Masaitis, 2006 ). ...
FIGURES | View All (12)
Image
Distribution of paleomagnetic poles in the zone of the dynamic influence of...
Published: 01 October 2018
Fig. 5. Distribution of paleomagnetic poles in the zone of the dynamic influence of the Vilyui paleorift system. 1 , dike swarms (1, Vilyui–Markha; 2, Kontai–Dzherba; 3, CharaSinsk); 2 , apparent polar wander path of the Siberian platform, after Torsvik et al. (2012) , numbers—geological age
Journal Article
Published: 01 October 2018
Russ. Geol. Geophys. (2018) 59 (10): 1217–1236.
..., the Vilyui–Markha swarm (750–800 km long and 125–150 km wide), CharaSinsk (northwestern branch: 250 km long and 175 km wide; southeastern branch: 450– 500 km long and 225 km wide). The Kontai–Dzherba field of dikes and sills (250 km long and 85–90 km wide), in which dikes strike NE, occurs...
FIGURES | View All (11)
Journal Article
Published: 01 September 2024
Russ. Geol. Geophys. (2024) 65 (9): 1052–1061.
... 99.58 99.60 99.52 99.54 100.24 100 100.63 100.30 100.30 100.10 n 3 2 5 3 1 3 2 3 7 6 5 7 9 Fig. 7. Geological map of the Kyulenke Rv. area. The CharaSinsk dike swarm has also attracted much practical interest ( Fig. 1 ) since we identified within its...
FIGURES | View All (7)