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  • ...downdip termination ([[:file:sedimentary-basin-analysis_fig4-57.png|Figure 4C]]). East-to-west reflection amplitude termination is stratigraphically cont ...amplitude anomalies ([[:File:Sedimentary-basin-analysis fig4-57.png|Figure 4C]]). The depositional model for a depositional [[dip]]-oriented gravity-flow
    8 KB (1,015 words) - 16:59, 23 March 2022
  • ...ata-to-subsurface-stratigraphic-and-structural-information_fig4.png|Figure 4c]]), is derived by placing the interval depths (MD<sub>i</sub>, MD<sub>''i''
    17 KB (2,363 words) - 16:49, 20 January 2022
  • ...nt for the clinoforms, ''P<sub>o</sub>'' ([[:File:BLTN13190fig4.jpg|Figure 4C]]). This provides flexibility in determining where to place the initial cli ...oform insertion point, ''P<sub>o</sub>'' ([[:File:BLTN13190fig4.jpg|Figure 4C]]), was qualitatively matched with a plan-view map of facies association be
    113 KB (16,689 words) - 22:11, 15 January 2024
  • ...pples capped by contorted laminations are common ([[:file:M31F5.jpg|Figure 4C]]). Deposition of 1 to 2 m can take place over only a few hours to a day. M
    33 KB (4,905 words) - 16:40, 6 April 2016