林小偉
listric normal fault
林小偉
Listric normal faults form during rifting, drifting, and evolution of passive continental margins with concomitant basinal development.
林小偉
Listric faults confined to the sedimentary prism are common features on passive margins, especially in progradational, post-evaporite sequences.
林小偉
https://images.plurk.com/4sayvuTHkZIEYgZe22DoYO.png
林小偉
林小偉
https://images.plurk.com/4h6EXqbuZUaxOCYovNgIUm.png
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