Особенности гидротермального и гипергенного изменения слюдистых кимберлитов

N. N. Zinchuk

Аннотация


На основании комплексного исследования акцессорных и породообразующих минералов кимберлитовых пород трубок Удачная, Нюрбинская и Ботуобинская детально прослежены процессы вторичного минералообразования. Изучены продукты изменения кимберлитовых пород, составлена схема преобразования исходных минералов, определены типоморфные особенности конечных продуктов выветривания, построен профиль коры выветривания кимберлитовых пород Накынского поля. Сравнительное комплексное исследование древних кор выветривания на породах различного химического и минералогического состава позволило проследить особенности их гипергенного изменения и типоморфные признаки элювиальных продуктов, что очень важно для решения ряда прикладных задач. В переотложенных продуктах выветривания различных пород возможно дифференцировать на структурном уровне одни и те же разновидности первичных минералов, а также идентифицировать вторичные слоистые силикаты, различающиеся в последнем случае либо характером заселения октаэдрических позиций в их структуре, либо способом взаимного наложения отдельных силикатных слоев или их политипией. Поэтому переотложенные в древних осадочных толщах продукты различных типов кор выветривания сохраняют структурные и кристаллохимические особенности по отношению к минералам элювиальных толщ, что позволяет проследить пути поступления в бассейны седиментации терригенного (в том числе и алмазоносного) материала.

Ключевые слова


древние коры выветривания; гипогенные и гипергенные минералы; типоморфизм минералов; алмазоносные толщи

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.22.1.32

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