Tectonophysics

Figure 1 and Figure 3 are the original .ai figures summarizing all the hydrological changes associated to the 1805 and 1930 earthquakes. The two .kml datasets plot the distribution of the hydrological changes associated to the 1805 and 1930 earthquakes in Google Earth.

The attached files correspond to supplementary material with the data used in the MT model shown in this work. Data consist on TE and TM apparent resistivity and phase for each measured sounding and MT inversion model responses (curves). The location of each MT sounding is presented in Figures 1 (Pz1 and Pz2) and 3,

Three-dimensional resistivity model produced by ModEM inversion

The S receiver functions from 51 permanent broad-band stations in study region and The earthquake catalogue in article collected from the Chinese State Seismological Scientific Data Sharing Center.

Data of quantitative morphology and terrestrial cosmogenic 36Cl dating. Please download it freely, if you are interested.

The original data of ASR in-situ stress measurement method.

The data are not the original data. The data are from Park, J.C., et al., 2007, Focal mechanisms of recent earthquakes in the Southern Korean Peninsula, Geophys. J. Int., 169. 1103-1114, Hong, T.K., Choi, H., 2012, Seismological constraints on the collision belt between the North and South China blocks in the Yellow Sea, Tectonophysics, 570, 102–113, and NIED F-net, 2019, National Research Institute for Earth Science and Disaster Resilience. https://doi:10.17598/NIED.0005.

Dataset of processed major-element composition of phengite, chlorite, epidote, feldspar, and biotite analyzed in samples FC1723, FC1727, FC1749, and FC1757, from Chilean Southern Patagonia (latitudes 52-54°S), in a field work in 2017 under the supervision of Prof. Mauricio Calderón. The mineral chemical composition was determined using the EPMA CAMECA SX100 at Universität Stuttgart, with 5 wavelength-dispersive spectrometers and an energy-dispersive system. Operating conditions were an acceleration voltage of 15 kV, a beam current of 15 nA, a beam size of 1–3 μm or a focused beam (for very small crystals), and 20 seconds counting time on the Kα peak (Ba: Lα) and on the background for each element. The standards used were natural wollastonite (Si, Ca), natural orthoclase (K), natural albite (Na), natural rhodonite (Mn), synthetic Cr2O3 (Cr), synthetic TiO2 (Ti), natural hematite (Fe), natural baryte (Ba), synthetic MgO (Mg), synthetic Al2O3 (Al) and synthetic NiO (Ni). The PaP correction procedure provided by CAMECA was applied. Analytical errors of this method are given by Massonne (2012).

Tables containing estimates source mechanisms of earthquakes that occured in the Vrancea Seismic Zone between 2014 and 2020, and principal stress axes obtained from inverting all the known earthquake focal mechanisms in the crust and upper mantle in the area

The QTQt data includes all the thermal history modelling statistical outputs from QTQtThe AFT counting data includes track counting data, track lengths, and Dpar values of samples.