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MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION. / Gurova, Alexandra V.; Safonova, I. Yu; Savinsky, I. A. et al.

In: Geodynamics and Tectonophysics, Vol. 13, No. 5, 0673, 2022.

Research output: Contribution to journal › Article › peer-review

Harvard

Gurova, AV, Safonova, IY, Savinsky, IA, Antonyuk, RM & Orynbek, TZ 2022, 'MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION', Geodynamics and Tectonophysics, vol. 13, no. 5, 0673. https://doi.org/10.5800/GT-2022-13-5-0673

APA

Gurova, A. V., Safonova, I. Y., Savinsky, I. A., Antonyuk, R. M., & Orynbek, T. Z. (2022). MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION. Geodynamics and Tectonophysics, 13(5), [0673]. https://doi.org/10.5800/GT-2022-13-5-0673

Vancouver

Gurova AV, Safonova IY, Savinsky IA, Antonyuk RM, Orynbek TZ. MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION. Geodynamics and Tectonophysics. 2022;13(5):0673. doi: 10.5800/GT-2022-13-5-0673

Author

Gurova, Alexandra V. ; Safonova, I. Yu ; Savinsky, I. A. et al. / MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION. In: Geodynamics and Tectonophysics. 2022 ; Vol. 13, No. 5.

BibTeX

@article{d81f255fbfb94b92b95601c87a2ea782,
title = "MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION",
abstract = "The paper provides an overview of the geological structure and presents new data on petrography and geochemistry of igneous rocks of the Tekturmas accretionary complex (TAC). Consideration is being given to the age, petrogenesis and probable tectonic settings of formation of igneous rocks. It is shown that the TAC and adjacent ophiolite belt are parts of the Late Cambrian – Ordovician Pacific-type orogenic belt formed at an active margin of the Paleo-Asian Ocean. The TAC is dominated mainly by tholeiitic mafic igneous rocks (basalt, dolerite, gabbro). There are recognized three groups of rocks: high-Ti, medium-Ti and low-Ti. Geological and geochemical features of TAC igneous rocks suggest their formation in three tectonic settings: mid-ocean ridge (medium-Ti), oceanic island/seamount (high-Ti) and over subduction zones (low-Ti).",
keywords = "Central Asian Orogenic Belt, Late Cambrian, Ordovician, Paleo-Asian Ocean, geochemistry, ophiolites, petrography",
author = "Gurova, {Alexandra V.} and Safonova, {I. Yu} and Savinsky, {I. A.} and Antonyuk, {R. M.} and Orynbek, {T. Zh}",
note = "Публикация для корректировки.",
year = "2022",
doi = "10.5800/GT-2022-13-5-0673",
language = "English",
volume = "13",
journal = "Geodynamics and Tectonophysics",
issn = "2078-502X",
publisher = "Institute of the Earth's Crust",
number = "5",

}

RIS

TY - JOUR

T1 - MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION

AU - Gurova, Alexandra V.

AU - Safonova, I. Yu

AU - Savinsky, I. A.

AU - Antonyuk, R. M.

AU - Orynbek, T. Zh

N1 - Публикация для корректировки.

PY - 2022

Y1 - 2022

N2 - The paper provides an overview of the geological structure and presents new data on petrography and geochemistry of igneous rocks of the Tekturmas accretionary complex (TAC). Consideration is being given to the age, petrogenesis and probable tectonic settings of formation of igneous rocks. It is shown that the TAC and adjacent ophiolite belt are parts of the Late Cambrian – Ordovician Pacific-type orogenic belt formed at an active margin of the Paleo-Asian Ocean. The TAC is dominated mainly by tholeiitic mafic igneous rocks (basalt, dolerite, gabbro). There are recognized three groups of rocks: high-Ti, medium-Ti and low-Ti. Geological and geochemical features of TAC igneous rocks suggest their formation in three tectonic settings: mid-ocean ridge (medium-Ti), oceanic island/seamount (high-Ti) and over subduction zones (low-Ti).

AB - The paper provides an overview of the geological structure and presents new data on petrography and geochemistry of igneous rocks of the Tekturmas accretionary complex (TAC). Consideration is being given to the age, petrogenesis and probable tectonic settings of formation of igneous rocks. It is shown that the TAC and adjacent ophiolite belt are parts of the Late Cambrian – Ordovician Pacific-type orogenic belt formed at an active margin of the Paleo-Asian Ocean. The TAC is dominated mainly by tholeiitic mafic igneous rocks (basalt, dolerite, gabbro). There are recognized three groups of rocks: high-Ti, medium-Ti and low-Ti. Geological and geochemical features of TAC igneous rocks suggest their formation in three tectonic settings: mid-ocean ridge (medium-Ti), oceanic island/seamount (high-Ti) and over subduction zones (low-Ti).

KW - Central Asian Orogenic Belt

KW - Late Cambrian

KW - Ordovician

KW - Paleo-Asian Ocean

KW - geochemistry

KW - ophiolites

KW - petrography

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85149132429&origin=inward&txGid=d18c6a707c3c5d13a7b2e98eba4109e2

UR - https://www.mendeley.com/catalogue/533ccce0-5890-3231-998a-ce2ec23f84a3/

U2 - 10.5800/GT-2022-13-5-0673

DO - 10.5800/GT-2022-13-5-0673

M3 - Article

VL - 13

JO - Geodynamics and Tectonophysics

JF - Geodynamics and Tectonophysics

SN - 2078-502X

IS - 5

M1 - 0673

ER -

ID: 55718559