Zobrazeno 1 - 10
of 14
pro vyhledávání: '"A. V. Pilitsyna"'
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 3, Pp 533-536 (2017)
Ultramafic and mafic lithologies, attributed to the orogenic terranes and formed under ultrahigh-pressure (UHP) and high-pressure (HP) conditions, have been intensively studied for the last decades. It is mainly related to a particular significance o
Externí odkaz:
https://doaj.org/article/c6dc9b444eef4a11aac666ee4a095590
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 28-44 (2015)
In the structure of Anrakhai massif of Chu-Ili region (Southern Kazakhstan) metamoiphic formations of high-pressure conditions derivation (under eclogite facies field) were identified; the rocks are represented by eclogites and garnet clinopiroxenite
Externí odkaz:
https://doaj.org/article/211407921f01481181635c7379956563
Autor:
V. P. Kovach, E. V. Tolmacheva, Yu. V. Plotkina, A. V. Pilitsyna, B. V. Ermolaev, Andrey A. Tretyakov, Kuo-Lung Wang, A. B. Kotov, E. B. Sal’nikova, Hao-Yang Lee, Valentina Batanova, Kirill E. Degtyarev
Publikováno v:
Lithos. :115-140
Palaeoproterozoic amphibole-biotite orthogneisses with a protolith age of ~ 1840 Ma and Neoproterozoic muscovite-chlorite orthogneisses with an estimated protolith age of ~ 790 Ma have been identified in the structure of the Zheltau terrane (Southern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::680f12d608acc483c2bd1a909568ded1
https://doi.org/10.1016/j.lithos.2018.10.033
https://doi.org/10.1016/j.lithos.2018.10.033
Autor:
Valentina Batanova, Simon Cuthbert, Kirill E. Degtyarev, B. V. Ermolaev, Taisia A. Alifirova, Elena V. Kovalchuk, A. V. Pilitsyna, Andrey A. Tretyakov
Publikováno v:
Gondwana Research. 64:11-34
Spinel-bearing ultramafic rocks, metamorphosed in high-pressure conditions, are described from the metamorphic complexes of the western part of the Central Asian Orogenic Belt (CAOB) in the Chu-Yili region in Southern Kazakhstan. They comprise small
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6fbd6f8d9c7c47eed4ffd8b9b43e9f9
https://doi.org/10.1016/j.gr.2018.06.005
https://doi.org/10.1016/j.gr.2018.06.005
Publikováno v:
Doklady Earth Sciences. 483:1504-1509
The Sakmara Allochthon (Southern Urals) comprises a widely distributed folded stratum of rhyolites and ignimbrites, which are characterized by Nb–Zr–REE geochemical specification. This stratum overlies unconformably folded Paleozoic complexes, in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a69ce2aeb183c2fddc9228ba38451258
https://doi.org/10.1134/s1028334x18120164
https://doi.org/10.1134/s1028334x18120164
Autor:
Valentina Batanova, A. V. Pilitsyna, Kirill E. Degtyarev, Elena V. Kovalchuk, Simon Cuthbert, Andrey A. Tretyakov
Publikováno v:
Journal of Asian Earth Sciences. 153:325-345
The Anrakhai Metamorphic Complex (AMC), located in the SE part of the Chu-Ili Mountains of Southern Kazakhstan in the western part of Central Asian Orogenic Belt, exhibits occurrences of HP metamorphic rocks in the form of eclogites and garnet clinop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f82fd55f6e1a532c2ed669828721bce9
https://doi.org/10.1016/j.jseaes.2017.03.027
https://doi.org/10.1016/j.jseaes.2017.03.027
Autor:
A. V. Pilitsyna, Andrey A. Tretyakov, Kirill E. Degtyarev, Elena V. Kovalchuk, Taisia A. Alifirova
Publikováno v:
Doklady Earth Sciences. 476:982-985
Spinel peridotite, metamorphosed in high-pressure conditions, was first described within the Western part of the Central Asian Orogenic Belt. The spinel peridotite has the characteristics of Mg–Cr ultramafites indicating the mantle origin of its pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7261742323055fa7762271601d5d94c9
https://doi.org/10.1134/s1028334x17090069
https://doi.org/10.1134/s1028334x17090069
Publikováno v:
Geodinamika i Tektonofizika, Vol 8, Iss 3, Pp 533-536 (2017)
Ultramafic and mafic lithologies, attributed to the orogenic terranes and formed under ultrahigh-pressure (UHP) and high-pressure (HP) conditions, have been intensively studied for the last decades. It is mainly related to a particular significance o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02368243c037a7149a1484120bb302ef
https://doi.org/10.5800/gt-2017-8-3-0283
https://doi.org/10.5800/gt-2017-8-3-0283
Autor:
A. V. Pilitsyna, A. S. Yakubchuk, Marina Luchitskaya, Kirill E. Degtyarev, Andrey A. Tretyakov
Publikováno v:
Lithos. :105818
The Junggar-Balkhash region in the west of the Central Asian orogenic belt (САОВ) comprises Paleozoic flysch, dismembered ophiolites, cherts, basalts, and olistostromes within its accretionary wedges. The North Balkhash ophiolite zone hosts serpe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15d477234acdcc0cd0c3e6ef6fcc9443
https://doi.org/10.1016/j.lithos.2020.105818
https://doi.org/10.1016/j.lithos.2020.105818
Autor:
V. P. Kovach, Andrey A. Tretyakov, Kirill E. Degtyarev, S. Z. Yakovleva, A. B. Kotov, A. V. Pilitsyna, E. B. Sal’nikova
Publikováno v:
Doklady Earth Sciences. 467:236-240
A migmatite–gneiss complex made up of paraand orthogneisses and crystalline schists with bodies of ultrametagenic tonalites is distinguished in the basement of the northwestern part of the Chuya–Kendyktas Massif. ID-TIMS dating of accessory zirco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c16882ce43b433f8f05fa79f785d483
https://doi.org/10.1134/s1028334x16030156
https://doi.org/10.1134/s1028334x16030156