1887
  1. Home
  2. Conferences
  3. Conference Proceedings
  4. 56th EAEG Meeting
  5. Conference paper
PDF

Abstract

An interesting phenomenon above some classic geological structures can be observed on many seismic sections. Namely, a part of the seismic horizon appears downthrown by normal faults to a position deeper than the flanks. The downthrown part of the horizon is above the shallowest parts of the classic antiform.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201410227
1994-06-10
2024-04-16

  • From This Site

    /content/papers/10.3997/2214-4609.201410227
    dcterms_title,dcterms_subject,pub_keyword
    -contentType:Journal -contentType:Contributor -contentType:Concept -contentType:Institution
    10
    5
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410227
Loading

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error