Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
GEOLOGICAL AND MINERALOGICAL CONTROLS ON IRON SKARN FORMATION IN THE NORTHWESTERN BALKHASH REGION (CENTRAL KAZAKHSTAN). / Nygmanova, A. S.; Korobkin, V. V.; Buslov, M. M. и др.
в: Herald of the Kazakh-British Technical University, Том 23, № 2, 35, 2026, стр. 464-480.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - GEOLOGICAL AND MINERALOGICAL CONTROLS ON IRON SKARN FORMATION IN THE NORTHWESTERN BALKHASH REGION (CENTRAL KAZAKHSTAN)
AU - Nygmanova, A. S.
AU - Korobkin, V. V.
AU - Buslov, M. M.
AU - Chaklikov, A. Ye.
AU - Tulemissova, Zh. S.
AU - Koishibayev, S. M.
N1 - Nygmanova A.S., Korobkin V.V., Buslov M.M., Chaklikov A.Ye., Tulemissova Zh.S., Koishibayev S.M. GEOLOGICAL AND MINERALOGICAL CONTROLS ON IRON SKARN FORMATION IN THE NORTHWESTERN BALKHASH REGION (CENTRAL KAZAKHSTAN). Herald of the Kazakh-British Technical University. 2026;23(2):464-480. https://doi.org/10.55452/1998-6688-2026-23-2-464-480
PY - 2026
Y1 - 2026
N2 - A comprehensive study has identified the principal geological and mineralogical controls governing the formation of iron skarn deposits in the Northwestern Balkhash region, based on representative deposits such as Zhuantobe and Karaulken. Integrated analysis of geological mapping, mineralogical and petrographic observations, geochemical data, and geophysical interpretations demonstrates that skarn formation represents a multistage contact-metasomatic system controlled by magmatic, structural, and fluid-related factors. Systematic patterns in the distribution of mineral assemblages and ore textural-structural types have been established, reflecting variations in fluid regimes and physicochemical conditions of ore formation. The obtained results refine the regional genetic model of iron skarn formation in the Northwestern Balkhash region and can be applied to the prediction and evaluation of the exploration potential of new ore targets.
AB - A comprehensive study has identified the principal geological and mineralogical controls governing the formation of iron skarn deposits in the Northwestern Balkhash region, based on representative deposits such as Zhuantobe and Karaulken. Integrated analysis of geological mapping, mineralogical and petrographic observations, geochemical data, and geophysical interpretations demonstrates that skarn formation represents a multistage contact-metasomatic system controlled by magmatic, structural, and fluid-related factors. Systematic patterns in the distribution of mineral assemblages and ore textural-structural types have been established, reflecting variations in fluid regimes and physicochemical conditions of ore formation. The obtained results refine the regional genetic model of iron skarn formation in the Northwestern Balkhash region and can be applied to the prediction and evaluation of the exploration potential of new ore targets.
KW - скарновые месторождения
KW - магнетитовые руды
KW - контактный метасоматоз
KW - минералогия
KW - геофизические аномалии
KW - Северо-Западное Прибалхашье
KW - skarn deposits
KW - magnetite ores
KW - contact metasomatism
KW - mineralogy
KW - geophysical anomalies
KW - Northwestern Balkhash region
UR - https://www.scopus.com/pages/publications/105044046933
UR - https://www.mendeley.com/catalogue/46ce4273-53f0-39a4-8940-2d6adb6d372b/
U2 - 10.55452/1998-6688-2026-23-2-464-480
DO - 10.55452/1998-6688-2026-23-2-464-480
M3 - Article
VL - 23
SP - 464
EP - 480
JO - Вестник Казахстанско-Британского технического университета
JF - Вестник Казахстанско-Британского технического университета
SN - 1998-6688
IS - 2
M1 - 35
ER -
ID: 81148992