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УДК 550.42: 552.3

https://doi.org/10.26516/2541-9641.2025.3.94

EDN: VIBTBF

Контрастная эволюция тектоносферы Индии и Северной Азии: Pb-изотопные датировки глубинных источников щелочных магматических комплексов с карбонатитами и Ba–Sr отношения пород

С.В. Рассказов1,2, Т.А. Ясныгина1, И.С. Чувашова1, Е.В. Саранина1,3

1Институт земной коры СО РАН, г. Иркутск, Россия

2Иркутский государственный университет, г. Иркутск, Россия

3 Институт геохимии им. А.П. Виноградова СО РАН, г. Иркутск, Россия

Аннотация. Для оценки сходства и различия источников карбонатитового магматизма в Индии и Северной Азии, неопротерозойские массивы Самалпатти и Севаттур и мел-палеогеновый массив Амба Донгар Индии сравниваются с неопротерозойско-раннепалеозойским массивом Томтор и меловыми массивами, Мало-Мурунским и Вэйшань – Северной Азии. Из Pb-изотопных данных по карбонатитам делается вывод о том, что карбонатитовые расплавы Самалпатти возрастом 800 млн лет были производными протолита мантийного источника возрастом около 4.26 млрд лет ранней Земли, который значительно отличался от первичного мантийного резервуара в затвердевшем магматическом океане по низкому начальному μ. После отделения Индийского субконтинента от Гондваны и его соединения с Азией силикатные расплавы крупной магматической провинции Декан генерировались из протолитов возрастом около 2 млрд лет средней геодинамической эпохи эволюции Земли. Карбонатиты Амба Донгар возрастом 66 млн лет были производными протолитов мантии ранней Земли, частично измененных событием возрастом около 2 млрд лет. Меловые карбонатиты массивов Мало-Мурунский и Вэйшань генерировались из протолитов, соответственно, 3.45 и 2.2 млрд лет. Карбонатитовый магматизм не проявился в Северной Азии в новейший геодинамический этап (т.е. в последние 90 млн лет), а роль карбонатитов в Индии постоянно возрастала. В это время тектоносфера Северной Азии подверглась перестройке, которая привела к подъему первичного материала Земли из глубинной мантии. Различный возраст протолитов и различное время формирования карбонатитов в Индии и Северной Азии подчеркиваются наследованием BaSr компонентов в древних и молодых карбонатитах Индии и специфическими трендами Ba и Sr в древних и молодых карбонатитах Северной Азии.

Ключевые слова: карбонатиты, нефелиновые сиениты, неопротерозой, мел, палеоген, Ba, Sr, микроэлементы, 206Pb/204Pb, 207Pb/204Pb, 143Nd/144Nd, 87Sr/86Sr, Индия, Северная Азия

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Rasskazov Sergei,

doctor of geological and mineralogical sciences, professor,

664033, Irkutsk, Lermontov st., 128,

Institute of the Earth's Crust SB RAS,

Head of the Laboratory for Isotopic and Geochronological Studies,

664025, Irkutsk, Lenin st., 3,

Irkutsk State University, Faculty of Geology,

Head of Dynamic Geology Char,

tel.: (3952) 51–16–59,

email: rassk@crust.irk.ru

 

Yasnygina Tatyana,

candidate of geological and mineralogical sciences,

664033, Irkutsk, Lermontov st., 128,

Institute of the Earth's Crust SB RAS,

Senior Researcher,

tel.: (3952) 51–16–59,

email: ty@crust.irk.ru

 

Chuvashova Irina,

candidate of geological and mineralogical sciences,

664033, Irkutsk, Lermontov st., 128,

Institute of the Earth's Crust SB RAS,

Senior Researcher,

664025, Irkutsk, Lenin st., 3,

Irkutsk State University, Faculty of Geology,

Associate Professor of Dynamic Geology Char,

tel.: (3952) 51–16–59,

email: chuvashova@crust.irk.ru

 

Saranina Elena,

candidate of geological and mineralogical sciences,

664033, Irkutsk, Lermontov st., 128,

Institute of the Earth's Crust SB RAS,

Lead Engineer,

664033, Irkutsk, Favorsky st., 1A, A.P. Vinogradov Institute of Geochemistry SB RAS,

email: e_v_sar@mail.ru

 

 

 



* Статья получена: 07.09.2025; исправлена: 14.09.2025; принята: 26.09.2025.

ДЛЯ ЦИТИРОВАНИЯ: Рассказов С.В., Ясныгина, Чувашова И.С., Саранина Е.В. Контрастная эволюция тектоносферы Индии и Северной Азии: Pb-изотопные датировки глубинных источников щелочных магматических комплексов с карбонатитами и Ba–Sr отношения пород // Геология и окружающая среда. 2025. Т. 5, № 3. С. 94–125. DOI 10.26516/2541-9641.2025.3.94. EDN: VIBTBF


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