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Impacts of data sampling on the interpretation of normal fault propagation and segment linkage
Tao, Ze ; Alves, Tiago M.
Tectonophysics, 2019-07, Vol.762, p.79-96
[Periódico revisado por pares]
Amsterdam: Elsevier B.V
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Título:
Impacts of data sampling on the interpretation of normal fault propagation and segment linkage
Autor:
Tao, Ze
;
Alves, Tiago M.
Assuntos:
Data
;
Data sampling
;
Data sampling interval
;
Earthquake damage
;
Fault lines
;
Fault propagation models
;
Faults
;
Geological faults
;
Geologists
;
Growth
;
Interpreters
;
Leakage
;
Normal faults, fault growth
;
Outcrops
;
Sampling
;
Sampling errors
;
Scaling
;
Segmentation
;
Slip
É parte de:
Tectonophysics, 2019-07, Vol.762, p.79-96
Descrição:
Throw-distance (T-D) and throw-depth (T-Z) plots are widely used by researchers and industry to examine the growth of normal faults. This study uses high-quality three-dimensional (3D) seismic and outcrop information to review the effect of data sampling on the interpretation of normal fault growth. The results show that the accuracy of T-D and T-Z data, and of resulting fault slip tendency and leakage factor analyses, are dependent on the sampling strategy followed by interpreters and field geologists, i.e. on a Sampling Interval/Fault Length Ratio (δ) for discrete structures. In particular, this work demonstrates that significant geometric changes in T-D plots occur when a Module Error (εi) for the ratio δ is larger than 6%–9% for faults of all scales and growth histories. This implies that a minimum number of measurements should be gathered on discrete faults to produce accurate T-D and T-Z plots, and that the number of measurements is dependent on fault length. With no prior knowledge of fault segmentation, a δ value of 0.05 should be applied when interpreting faults to fulfil the pre-requisite of a ɛi < 6–9%. In all faults analysed, slip tendency and leakage factors were systematically misrepresented with increasing δ values. To disregard the limits proposed in this work results in: 1) a systematic underrepresentation of the isolated fault growth model, 2) a systematic misrepresentation of fault geometries and related damage zones, 3) the collation of erroneous fault scaling relationships, and 4) ultimately, unreliable interpretations of fault sealing properties. Hence, this work presents a new tool for interpreters and structural geologists to understand the sampling strategies necessary to obtain accurate fault throw and displacement data at different scales of analysis. •We present a new tool to understand the sampling strategies necessary to obtain reliable fault displacement data at different scales of analysis;•The accuracy of T-D and T-Z data, and of resulting fault slip tendency and leakage factor analyses, are dependent on the sampling strategy;•Significant errors in T-D plots occur when sampling intervals exceed 5% of the total length of segmented faults;•Fault stress analyses require sampling intervals approaching maximum data resolution.
Editor:
Amsterdam: Elsevier B.V
Idioma:
Inglês
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