Stratal architecture and origin of lateral accretion deposits (LADs) and conterminuous inner-bank levee deposits in a base-of-slope sinuous channel, lower Isaac Formation (Neoproterozoic), East-Central British Columbia, Canada

R.W.C. Arnott، نويسنده ,

روزنامه با شماره پیاپی سال 2007

14

515

528

Turbidity inner-bend (point-bar) deposition , Sinuous channels , Lateral accretion deposits

Marine and Petroleum Geology

2007

Marine and Petroleum Geology

314359