Magnetic model of the crystalline crust and heterogeneity  of the lithosphere in the junction zones between  the East European Craton and surrounding structures.  Part I. The SW border

Інна Пашкевич; Михайло Орлюк; Марія Бакаржієва; Андрій Марченко

doi:10.24028/gj.v48i1.347053

Автор(и)

Інна Пашкевич Інститут геофізики ім. С.І. Субботіна НАН України, Київ, Україна, Україна
Михайло Орлюк Інститут геофізики ім. С.І. Субботіна НАН України, Київ, Україна, Україна
Марія Бакаржієва Інститут геофізики ім. С.І. Субботіна НАН України, Київ, Україна, Україна
Андрій Марченко Інститут геофізики ім. С.І. Субботіна НАН України, Київ, Україна, Україна

DOI:

https://doi.org/10.24028/gj.v48i1.347053

Ключові слова:

Східноєвропейський кратон, 3D магнітне моделювання, магнітне поле, неоднорідність літосфери, магнітні аномалії, магматизм, лінія Тейссейра-Торнквіста, мантія, зони субдукції

Анотація

У статті вперше зроблено спробу встановити зв’язок магнітних неоднорідностей кристалічної кори в районі лінії Тейссейре—Торнквіста південно-західної окраїни Східноєвропейського кратона з неоднорідностями мантії. 3D магнітну модель кристалічної кори побудовано з використанням приземного аномального магнітного поля, швидкісних і структурних розрізів по сейсмічних профілях. Джерела віднесені до двох поверхів: локальні до всієї товщини верхньої кори, глибинні — до середньої і нижньої кори. Намагніченість прийнята однорідною, рівноважною і постійною до глибини розділу Мохо та досягнення температури Кюрі магнетиту. Така параметризація моделі призвела до оцінки мінімально можливих значень намагніченості джерел. Збіг сумарного ефекту корових джерел зі спостереженим полем досягався методом проб і помилок з похибкою, яка не перевищувала 30 нТ. Співвідношення корових магнітних неоднорідностей і структури мантії базується на використанні складених схем головних особливостей кристалічної кори, неоднорідності підкорової мантії та перехідного шару від верхньої до середньої мантії. Головною особливістю 3D магнітної моделі є наявність глибинних магнітних тіл, супутніх лінії Тейссейре—Торнквіста, зоні Соргенфрей—Торнквіста і шву Тор—Торнквіста. Смуга магнітних тіл з північного сходу обмежена субпаралельним лінії Тейссейре—Торнквіста лінеаментом L, виділеним нами за структурою магнітного поля. Він корелює з деформаційним фронтом Каледонід у Фенноскандії та Рава-Руським розломом у Сарматії. Це дає змогу пов’язати магнітні джерела з активізацією системи лінії Тейссейре—Торнквіста та мафічними інтрузіями. Про магматичний генезис даних магнітних джерел свідчить також положення їх над насувом підкорової мантії Східноєвропейського кратона на мантію Західноєвропейської платформи. Насув встановлений за даними сейсмотомографії. Він корелює з підсувом нижньої кори Східноєвропейського кратона під кору Західноєвропейської платформи. Передбачається зв’язок цих структур із синхронним рухом їх із північного сходу на південний захід, формуванням зони розтягування та інтрузій. Режим розтягування вздовж лінії Тейссейре—Торнквіста може також бути обумовленим південно-західною субдукцією, що підтверджують виділені високошвидкісні похилі шари (слеби). Магматичне походження магнітних джерел не виключає утворення «вторинних» магнітних мінералів унаслідок проникнення в кристалічну кору глибинних флюїдів. Цьому процесу сприяє підвищена проникність літосфери, «розмитість» головної геодинамічної межі, порушення структури перехідного шару верхньої мантії. Природа глибинних магнітних джерел, пов’язаних з лінією Тейссейре—Торнквіста, пояснюється таким чином як первинними магнітними мінералами мафічних порід, так і вторинними, привнесеними з глибин.

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