Структурні особливості літосфери континентів і океанів та їх природа

Автор(и)

  • N. I. Pavlenkova Інститут фізики Землі ім. О. Ю. Шмідта РАН, Російська Федерація

DOI:

https://doi.org/10.24028/gzh.0203-3100.v41i2.2019.164448

Ключові слова:

глибинна геофізика, земна кора, верхня мантія, петрофізика, глибинні флюїди, глобальні порушення, дегазація і розширення Землі

Анотація

Глибинними геолого-геофізичними дослідженнями континентів і океанів виявлено такі добре обґрунтовані закономірності у структурі земної кори і верхньої мантії, які не мають чіткого пояснення в сучасних геодинамічних концепціях. Земля розділена на дві півкулі з різною структурою літосфери — Тихоокеанську й Індо-Атлантичну, що розмежовані кільцем тектонічно активних зон високої сейсмічності (зонами Беньофа). Система серединно-океанічних хребтів з приблизно однаковими відстанями між ними (90°) симетрична щодо Південного полюса. Кора в океанах різниться за віком і складом, виділено залишки давньої (архейської) кори і великі площі субконтинентальної кори. Континенти характеризуються великою потужністю літосфери (понад 200 км), складеної деплетованим матеріалом зменшеної густини. Згідно з експериментальними даними щодопетрофізичнихвластивостей речовини земної кори і верхньої мантії за високого тиску і температури, а також даними стосовно глибинних ксенолітів і геохімічнихдосліджень природних газів, роль глибоких енергоємних флюїдів у формуванні сіалічної кори і деплетованої мантії є великою. Природу формування континентів і океанів можна пояснити таким чином. Нерівномірна за площею дегазація Землі привела до утворення різних типів літосфери: потужна граніто-гнейсовa кора і деплетована мантія зменшеної густини формувалися в зонах підвищених потоків глибинних флюїдів, а в зонах зниженої флюїдної адвекції зберігалася первинна океанічна кора й утворювалися лише невеликі ділянки кори перехідного типу. Наявність «коренів» континентів зі зменшеною густиною була основною причиною формування континентів: літосфера зменшеної густини «спливла» щодо океанічної літосфери. Дві півкулі з різною структурою літосфери утворилися, ймовірно, в результаті обертання Землі по орбіті еліпсоїдальної форми, що викликає періодичні коливання планети. Структурну симетрію глобальної системи рифтів щодо полюсів планети можна пояснити розширенням планети.

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2019-04-17

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Pavlenkova, N. I. (2019). Структурні особливості літосфери континентів і океанів та їх природа. Геофізичний журнал, 41(2), 3–57. https://doi.org/10.24028/gzh.0203-3100.v41i2.2019.164448

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