Understanding compaction localization in porous limestone in the laboratory is significantly more challenging than in sandstone because of the lack of consistent acoustic emission activity in carbonate samples. Previous studies have therefore relied on X-ray Computed Tomography imaging (CT). The first unambiguous evidence of compaction band development in limestone was provided by Huang et al. (2019), who performed synchrotron in situ CT imaging during shear-enhanced compaction in a sample of Leitha limestone. In this study, we analyzed this data set using Digital Volume Correlation (DVC). Our new results confirm that inelastic compaction occurred in two stages in Leitha limestone: macropore collapse first and then sequential growth of compaction bands. The displacement field inferred from DVC revealed that the bands in Leitha limestone showed mostly normal displacement discontinuities, as expected for compaction bands. DVC analysis also gave more constraints on band geometric attributes, as well as on the spatiotemporal development of strain. Analysis of the autocorrelation function for the volumetric strain suggests spatiotemporal correlation of strain precursory to the band's formation, their width, spacing and their complex sequential growth.