التفاصيل البيبلوغرافية
| العنوان: |
Дислокации в четвертичных отложениях Балтийского Щита, Русской плиты и Северо-Восточной Якутии |
| المؤلفون: |
Горбатов Е.С., Рассказов А.А., Колесников С.Ф. |
| المصدر: |
Бюллетень Комиссии по изучению четвертичного периода |
| المجموعة: |
RUDN University Open Repository (RUOR) |
| مصطلحات موضوعية: |
deformation structures, Convolutions, faults dislocations, ground veins, shell structures, typification, formation mechanisms, limnogenic complexes, East European Platform, yakutia, деформационные структуры, конволюции, разрывные дислокации, грунтовые жилы, структуры облекания, типизация, механизмы формирования, лимногенные комплексы, Восточно-Европейская платформа, якутия |
| الوصف: |
In limnogenic, fluvio- and limnoglacial late Pleistocene deposits of the Baltic Shield and the Russian Plate and limnogenic (alas) complexes of different ages in North-Eastern Yakutia, which were formed under conditions of different levels of activity of seismotectonic, glacial and cryogenic processes, identified various types of dislocations (structures of soil liquefaction or convolutions, underwater slump folds, faults, ground veins, etc.). On the basis of the collected lithological material (20 sections), by comparing the prevalence of disturbances of each type with each other, their different genesis is shown. Convolute disturbances are present in three regions, which may indicate different mechanisms of their formation (gravitational instability, cryogenesis, seismic liquefaction). These structures are morphologically similar to seismites and are sometimes mistaken for traces of paleoearthquakes; however, in the studied periglacial regions, they appear only in sedimentary systems with low dynamic stability. Therefore, the probability of their seismic initiation is relatively low. Vergent slump folds are distributed locally in areas of mountainous relief (khibiny massif). Faults are most characteristic of glacial deposits; they do not show activity in the post-glacial period and may be associated with subsidence or settlement of strata in the body of the sheet glacier and subsequent landslide processes. ground veins and shell structures to the greatest extent reflect the activity of cryogenic processes. The results obtained significantly expand the understanding of the conditions for the formation of soil disturbances in Quaternary deposits. ; В лимногенных, флювио- и лимногляциальных позднеплейстоценовых отложениях Балтийского щита и Русской плиты и лимногенных (аласных) разновозрастных комплексах Северо-Восточной Якутии, формирование которых происходило в условиях разного уровня активности сейсмотектонических, гляциальных и криогенных процессов, широко распространены различные типы дислокаций (структуры ... |
| نوع الوثيقة: |
article in journal/newspaper |
| اللغة: |
Russian |
| العلاقة: |
https://repository.rudn.ru/records/article/record/100467Test/ |
| الإتاحة: |
https://repository.rudn.ru/records/article/record/100467Test/ |
| رقم الانضمام: |
edsbas.9F81A82A |
| قاعدة البيانات: |
BASE |
