Page 174 - The Petroleum System From Source to Trap
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166     Deming


                                                   AGE(Ma)
                                                200           100            0
                            w
                            �
                            w
                            0    2
                            �
                            :::J  E  3
                            CIJ ->::
                            0    4
                            �       1000
                            1-   5
                                 6

                                                   AGE (Ma)
                                 300            200           1 0 0          0
                                 0 �--��--����----�--����


                                 3  �                   �
                                 2

                             �                            �
                                 4
                                 5                     P A SSIVE MARGINS

                                 6
                                  ������==�==�==�
                                 600            500           400           300
                                                                                Sallnlan t.ln
                                        AGE (Ma)
                                 500            400           300


                                                        -.;;;;;;;::
                          2                        Williston Basin   2
                          3                                          3
                      �                                          �
                          4             INTRACRATONIC BASINS         4
                          5                                          5
                          6 �--�-----=�=�                            6



                                                                        AGE (Ma)
                                                                                  0



                           2
                           3
                       �
                           4
                                 CE    FORELAND BASINS
                           5                                      5
                                   9 � �
                                      � 100
                          6               ,                       6
                                  500           400


          Figure 9.1. Representative tectonic subsidence histories for basins from different tectonic settings. The top graph shows the
          slopes of a range of sedimentation rates after compaction and is provided for reference. (After Angevine et al., 1990.)
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