Supporting Data: Linking Geodetically Resolved Uplift to Long-Term Orogenic Exhumation in the Southern Alps, New Zealand

This is the supporting data for Linking Geodetically Resolved Uplift to Long-Term Orogenic Exhumation in the Southern Alps, New Zealand. This supporting information includes datasets in .txt format of InSAR LOS velocities for each frame and the 3-component velocity fields over the central Southern Alps, New Zealand, the data used for fault inversion, and a .grd file of the resulting exhumation proxy. Data Sets DS1–DS4: LOS Velocities (D1-4 LOS StaMPS velocities/)D1–4 are the LOS velocities for tracks 023A, 125A, 044D, and 146D respectively. These have been corrected for DEM error and atmosphere, and downsampled to a 0.5 km resolution (Hooper et al., 2012; Bekaert et al., 2015). They are provided as a 7 column textfile, where columns are 1) Longitude (degrees), 2) Latitude (Degrees), 3) LOS Velocity (mm/yr 4) Velocity STD (mm/yr), 5) Satellite Azimuth (degrees), 6) Incidence angle (degrees), 7) Height of pixel Data Set DS5: ENU Velocities (D5 ENU velocity.txt)East, north and up velocities (Fig. S2), where the GNSS north velocity (Beavan et al., 2016) is first removed from LOS before inverting for east and up (Wright et al.,2004). A vertical GNSS transect (Beavan et al., 2010) was then used to reference the up velocities. These are provided in a 10 column textfile where columnsare 1) Longitude (degrees), 2) Latitude (degrees), 3–4) East velocity and error (mm/yr), 5–6) North velocity and error (mm/yr), 7–9) Unreferenced and referenced up velocity and error (mm/yr), and 10) Pixel Height (m). Data Set DS6: GBIS Profiles (D6 GBIS/)This folder contains ENU velocities for each profile in a format ready for GBIS inversion (Bagnardi & Hooper, 2018). Also included are is the edited version of GBIS (GBIS V1.2)used to invert for fault structure, including new model arrangements and the config files needed to run GBIS. Data Set DS7: Exhumation Proxy (D7 proxyExhumation.grd) Exhumation proxy created by adding the tGISU and modelled coseismic displacements in GMT 6.2.0 (Wessel et al., 2019). Provided as a .grd file, following application of a 2 × 2 km spatial filter.