USING T-Z PLOTS AS A GRAPHICAL METHOD TO INFER LITHOLOGICAL VARIATIONS FROM GROWTH STRATA
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dc.contributor.author | Castelltort S. | |
dc.contributor.author | Pochat S. | |
dc.contributor.author | Van Den Driessche J. | |
dc.date.accessioned | 2022-10-07T08:40:42Z | |
dc.date.available | 2022-10-07T08:40:42Z | |
dc.date.issued | 2004 | |
dc.identifier | https://elibrary.ru/item.asp?id=14022089 | |
dc.identifier.citation | Journal of Structural Geology, 2004, 26, 8, 1425-1432 | |
dc.identifier.issn | 0191-8141 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38912 | |
dc.description.abstract | The ’T–Z plot’ method consists of plotting the throw of sedimentary horizons across a growth fault versus their depth in the hanging wall. This method has been initially developed for the analysis of growth fault kinematics from seismic data. A brief analytical examination of such plots shows that they can also provide valuable information about the evolution of fault topography. When growth is a continuous process, stages of topography creation (fault scarp) and filling (of the space available in the hanging-wall) are related to non-dynamic (draping, mud-prone pelagic settling) and dynamic (sand-prone, dynamically deposited) sedimentation, respectively. In this case, the T–Z plot analysis becomes a powerful tool to predict major lithological variations on seismic profiles in faulted settings. | |
dc.subject | Growth fault | |
dc.subject | Growth strata | |
dc.subject | Fault-generated topography | |
dc.subject | Fault kinematics | |
dc.subject | Net-to-gross ratio | |
dc.title | USING T-Z PLOTS AS A GRAPHICAL METHOD TO INFER LITHOLOGICAL VARIATIONS FROM GROWTH STRATA | |
dc.type | Статья |
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