Recognizing the threshold magnetic anisotropy for inclination shallowing: Implications for correcting inclination errors of sedimentary rocks
Post-depositional compaction is an integral part of sedimentary rock formation and thus has been reasonably deemed as a major culprit for the long-recognized inclination-shallowing problem in sedimentary rocks. Although theoretical treatment elegantly envisions magnetic anisotropy (or oblate fabrics...
| 發表在: | Frontiers in Earth Science |
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| Main Authors: | , , , |
| 格式: | Article |
| 語言: | 英语 |
| 出版: |
Frontiers Media S.A.
2014-05-01
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| 主題: | |
| 在線閱讀: | http://journal.frontiersin.org/Journal/10.3389/feart.2014.00008/full |
