Title of article
Marine terraces of Western Sakhalin Island
Author/Authors
Korotky، نويسنده , , Aleksey and Grebennikova، نويسنده , , Tatyana and Razjigaeva، نويسنده , , Nadya and Volkov، نويسنده , , Victor and Mokhova، نويسنده , , Ludmila and Ganzey، نويسنده , , Larisa and Bazarova، نويسنده , , Valya Vassileva، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 1997
Pages
21
From page
61
To page
81
Abstract
Biostratigraphical and sedimentological studies of deposits of terraces with heights of 2–3, 3–4, 4–6, 8–10, 12–15, 20–30, 35–40, 60–80 and 100–120 m on Western Sakhalin Island have shown that they were all marine in origin. The upper complex of terraces (QI–QII) formed during a period of slow tectonic uplift (< 0.1 m ka− in this area to 120 m above modern sea level. The lower complex of terraces (QIII–QIV) may have formed in response to sea level oscillations without any influence of tectonic uplift.
Keywords
Biostratigraphical , Sedimentological , Marine terraces
Journal title
CATENA
Serial Year
1997
Journal title
CATENA
Record number
2251356
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