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| Content Provider | Springer Nature Link |
|---|---|
| Author | Sorokin, A. A. Buchko, I. V. Kotov, A. B. Velikoslavinsky, S. D. |
| Copyright Year | 2010 |
| Abstract | The Baladek Massif represents a tectonic block located at the boundary between the SE framing of the North Asian craton and the fold structures of the Galam terrane of the Mongol-Okhotsk fold belt. According to the existing concepts, the rocks of this massif are regarded as Precambrian complexes of the aforementioned craton. This paper reports the results of studying the fragment of the Baladek Massif in the Gerbikan River basin. New geochemical data obtained on the gabbros, gabbroanorthosites, and ultramafic rocks testify to their similarity with typical ophiolite complexes. An underlying complex of metamorphic ultrabasic rocks, a layered complex of pyroxenites and “cumulate” gabbros, gabbroanorthosites, and a complex of isotropic gabbros were distinguished within this fragment. It is highly possible that the basic volcanic rocks and jaspers of the Silurian-Lower Devonian sequences of the Galam segment of the Mongol-Okhotsk fold belt also belong to the inferred ophiolite complex. |
| Starting Page | 418 |
| Ending Page | 428 |
| Page Count | 11 |
| File Format | |
| ISSN | 18197140 |
| Journal | Russian Journal of Pacific Geology |
| Volume Number | 4 |
| Issue Number | 5 |
| e-ISSN | 18197159 |
| Language | English |
| Publisher | SP MAIK Nauka/Interperiodica |
| Publisher Date | 2010-10-21 |
| Publisher Place | Dordrecht |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | gabbro-anorthosites ophiolites southeastern framing of the North Asian craton Baladek Massif Geology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geology Geophysics Geochemistry and Petrology Oceanography Paleontology Stratigraphy |
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