Analyzing structural variations along strike in a deep-water thrust belt. (March 2018)

• Record Type: Journal Article
• Authors: Totake, Yukitsugu; Butler, Robert W.H.; Bond, Clare E.; Aziz, Aznan
• Is Part Of: Journal of structural geology. Volume 108(2018)
• Page Start: 213
• Page End: 229
• Publication Date: 2018-03
• Subjects: Fold thrust belt -- Displacement analysis -- Fault linkage -- Strain localization -- Deep water -- Malaysia; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2017.06.007
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: We characterize a deep-water fold-thrust arrays imaged by a high-resolution 3D seismic dataset in the offshore NW Borneo, Malaysia, to understand the kinematics behind spatial arrangement of structural variations throughout the fold-thrust system. The seismic volume used covers two sub-parallel fold trains associated with a series of fore-thrusts and back-thrusts. We measured fault heave, shortening value, fold geometries (forelimb dip, interlimb angle and crest depth) along strike in individual fold trains. Heave plot on strike projection allows to identify individual thrust segments showing semi-elliptical to triangular to bimodal patterns, and linkages of these segments. The linkage sites are marked by local minima in cumulative heave. These local heave minima are compensated by additional structures, such as small imbricate thrusts and tight folds indicated by large forelimb dip and small interlimb angle. Complementary profiles of the shortening amount for the two fold trains result in smoother gradient of total shortening across the structures. We interpret this reflects kinematic interaction between two fold-thrust trains. This type of along-strike variation analysis provides comprehensive understanding of a fold-thrust system and may provide an interpretative strategy for inferring the presence of complex multiple faults in less well-imaged parts of seismic volumes. Graphical abstract: Image 1 Highlights: Fault heave changes along strike in a deep-water thrust belt, offshore Malaysia. Multiple heave maxima on the main thrusts suggest merger of fault segments. Fault linkage sites exhibiting local heave minima concur with distributed strain on small imbricate thrusts and tight folds. Fault linkage and displacement kinematics are affected by adjacent structures across strike. A fold-thrust structure may be better characterized as a part of kinematically linked 3D system.