geolmsuВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯMoscow University Bulletin. Series 4. Geology0579-9406Издательский Дом МГУ10.33623/0579-9406-2020-1-28-36geolmsu-217Research ArticleСтатьиРегенерационное железное оруденение на месторождении Сишимэнь (северо-восток Китая)Regeneration iron metallization at the Xishimen field (North-East China)СюйдунШиXudongShi

геологический факультет, кафедра геологии, геохимии и экономики полезных ископаемых, аспирант

119991, Москва, ГСП-1, Ленинские Горы, 1

119991, GSP-1, Leninskiye Gory, 1

sxdmsu@yandex.ruМосковский государственный университет имени М.В. ЛомоносоваРоссияLomonosov Moscow State UniversityRussian Federation202028022020012836Copyright © Сюйдун Ш., 20202020Сюйдун Ш.Xudong S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://vestnik.geol.msu.ru/jour/article/view/217

Скарновое железорудное месторождение Сишимень, приуроченное к глубинному разлому, расположено на контакте малых интрузий монцодиоритов с палеозойскомезозойскими карбонатными породами. Оно представлено несколькими залежами лентовидной и линзовидной формы. Образование руд связано с процессами рециклинга рудного вещества. Процесс протекал в несколько этапов. Первичные осадочные и вулканогенно-осадочные руды формировались в архее–нижнем протерозое. Затем по следовало несколько этапов тектономагматической активизации, среди которых наиболее значительным был аншанский (юрско-меловой). Монцодиоритовая магма в процессе рециклинга обогащалась сидерофильными элементами раннего докембрия и формировала в зоне глубинных разломов серию железорудных месторождений.

The Xishimen skarn iron deposit was confined to a deep fault and locates at the contact of small intrusions of monzodiorites with Pz–Mz carbonate rocks. It is represented by several banding and lenticular forms. The formation of ores is associated with the recycling processes of ore matter. The process proceeded in several stages. Primary sedimentary and volcanogenic-sedimentary ores were formed in Ar–Prt1 time. Then followed several stages of tectonic-magmatic activation, among which the most significant was Anshan stage (Jurassic-Cretaceous). Monzodiorite magma in the process of recycling was enriched by siderophilic elements of early Precambrian and formed a series of Fe deposits in the zone of deep faults.

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The authors declare that there are no conflicts of interest present.