This dataset contains the experimental measurements used to generate the figures and results presented in the manuscript "Geometry-Driven Convection in Sheared Packings of Spherical Particles", submitted to Physical Review Letters. The data are provided in Excel format and organized by figures in different sheets.

This dataset contains the experimental measurements used to generate the figures and results presented in the manuscript "Geometry-Driven Convection in Sheared Packings of Spherical Particles", submitted to Physical Review Letters. The data are provided in Excel format and organized by figures in different sheets.

Data set supporting diagrams presented in the manuscript entitled "Effects of strong, monovalent and short-ranged monomer-monomer interactions on the phase separation of polymeric macromolecules" from authors Masoud Mirzaei and Hossein Fazli which is beeng submitted for pubication.

Data set supporting diagrams presented in the manuscript entitled "Effects of strong, monovalent and short-ranged monomer-monomer interactions on the phase separation of polymeric macromolecules" from authors Masoud Mirzaei and Hossein Fazli which is beeng submitted for pubication.

Raw data used for plots in the main Figure (Fig. 2) of the paper "Entanglement entropy scaling laws from fluctuations of non-conserved quantities".   (a) Phase diagram - imbalance_spin_z archive contains files with site and corresponding S_z for each point in the phase diagram. correlations_x contains the full \langle S_x S_x \rangle correlation matrix. The paper contains information on how this raw data has been used to generate the spin imbalance and the correlator.(b) Conserved case fluctuations and entanglement entropy - entvar_xxz_jz0.250.dat with columns: chain length; von Neumann entropy; Renyi entropy; S_z fluctuations(c) Reduced fluctuations area law phase - entvar_gs_g0.30_jz1.00_areaMott.dat with columns: chain length; von Neumann entropy; Renyi entropy; S_z half system fluctuations; S_z full system fluctuations; S_x half system fluctuations; S_x full system fluctuations; S_y half system fluctuations; S_y full system fluctuations(d) & (e) Reduced fluctuations critical point - entvar_gs_g0.200_jz0.600.dat with same structure as (c)(f) visibility - visib_gs_Jz0.7.dat with same structure as (c), (d), (e). The paper contains information on how this raw data has been used to generate the visiblity for each spin direciton.

Raw data used for plots in the main Figure (Fig. 2) of the paper "Entanglement entropy scaling laws from fluctuations of non-conserved quantities".   (a) Phase diagram - imbalance_spin_z archive contains files with site and corresponding S_z for each point in the phase diagram. correlations_x contains the full \langle S_x S_x \rangle correlation matrix. The paper contains information on how this raw data has been used to generate the spin imbalance and the correlator.(b) Conserved case fluctuations and entanglement entropy - entvar_xxz_jz0.250.dat with columns: chain length; von Neumann entropy; Renyi entropy; S_z fluctuations(c) Reduced fluctuations area law phase - entvar_gs_g0.30_jz1.00_areaMott.dat with columns: chain length; von Neumann entropy; Renyi entropy; S_z half system fluctuations; S_z full system fluctuations; S_x half system fluctuations; S_x full system fluctuations; S_y half system fluctuations; S_y full system fluctuations(d) & (e) Reduced fluctuations critical point - entvar_gs_g0.200_jz0.600.dat with same structure as (c)(f) visibility - visib_gs_Jz0.7.dat with same structure as (c), (d), (e). The paper contains information on how this raw data has been used to generate the visiblity for each spin direciton.

The Makran Subduction Zone is unusual, with an ENE-WSW trending volcanic arc that is nonparallel to its ~E-W trending accretionary prism. The discrepancy has been attributed to an eastward reduction of the subduction angle. To assess this theory, we relocated 146 moderate to large earthquakes in the region during the period 1968 to 2022. We found that in eastern Makran, the region with intermediate-depth earthquakes has a constant width of ~180 km, with a trend sub-parallel with the trend of the volcanic arc. The fault planes of most of the normal-faulting intermediate-depth earthquakes are also parallel to the trend of the volcanic arc. These observations suggest an ENE-WSW trending subducting plate hinge and a constant subduction angle in eastern Makran. The ~E-W trend of the intermediate-depth earthquakes in western Makran indicates an ~E-W trending subducting plate hinge. We relate the different orientation of the plate hinges in eastern and western Makran to the different shape of the overriding plates. The cumulative Wadati-Benioff zone for eastern Makran shows a subduction angle of ~15o in the depth range of ~45-80 km, increasing to ~45o at depths greater than 80 km. The significant component of strike-slip faulting of the intermediate-depth events in western Makran implies that the subducting plate in western and eastern Makran experience different stress regimes. Alignment of a consid-erable number of intermediate-depth earthquakes along narrow ENE-WSW lineaments implies a pre-existing weakness in the subducting plate.

The Makran Subduction Zone is unusual, with an ENE-WSW trending volcanic arc that is nonparallel to its ~E-W trending accretionary prism. The discrepancy has been attributed to an eastward reduction of the subduction angle. To assess this theory, we relocated 146 moderate to large earthquakes in the region during the period 1968 to 2022. We found that in eastern Makran, the region with intermediate-depth earthquakes has a constant width of ~180 km, with a trend sub-parallel with the trend of the volcanic arc. The fault planes of most of the normal-faulting intermediate-depth earthquakes are also parallel to the trend of the volcanic arc. These observations suggest an ENE-WSW trending subducting plate hinge and a constant subduction angle in eastern Makran. The ~E-W trend of the intermediate-depth earthquakes in western Makran indicates an ~E-W trending subducting plate hinge. We relate the different orientation of the plate hinges in eastern and western Makran to the different shape of the overriding plates. The cumulative Wadati-Benioff zone for eastern Makran shows a subduction angle of ~15o in the depth range of ~45-80 km, increasing to ~45o at depths greater than 80 km. The significant component of strike-slip faulting of the intermediate-depth events in western Makran implies that the subducting plate in western and eastern Makran experience different stress regimes. Alignment of a consid-erable number of intermediate-depth earthquakes along narrow ENE-WSW lineaments implies a pre-existing weakness in the subducting plate.

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