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Thanks to the policy of BSSA, SRL and PRL, I could upload some published versions of the manuscripts I (co-) authored to induced.pl website. This includes the following papers:

Kwiatek, G., P. Martínez-Garzón, and M. Bohnhoff (2016). HybridMT: A MATLAB/Shell Environment Package for Seismic Moment Tensor Inversion and Refinement, Seismol. Res. Lett. 87, no. 4, 964–976, doi 10.1785/0220150251.

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Martínez-Garzón, P., G. Kwiatek, M. Ickrath, and M. Bohnhoff (2014). MSATSI: A MATLAB Package for Stress Inversion Combining Solid Classic Methodology, a New Simplified User- Handling, and a Visualization Tool, Seismol. Res. Lett. 85, no. 4, 896–904, doi 10.1785/0220130189.

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Davidsen, J., and G. Kwiatek (2013). Earthquake interevent time distribution for induced micro-, nano- and picoseismicity, Phys. Rev. Lett. 110, 068501, doi 10.1103/PhysRevLett.110.068501.

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Davidsen, J., G. Kwiatek, and G. Dresen (2012). No Evidence of Magnitude Clustering in an Aftershock Sequence of Nano- and Picoseismicity, Phys. Rev. Lett. 108, 038501, doi 10.1103/PhysRevLett.108.038501.

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Kwiatek, G., K. Plenkers, and G. Dresen (2011). Source Parameters of Picoseismicity Recorded at Mponeng Deep Gold Mine, South Africa: Implications for Scaling Relations, Bull. Seismol. Soc. Am. 101, no. 6, 2592–2608, doi 10.1785/0120110094.

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Plenkers, K., D. Schorlemmer, and G. Kwiatek (2011). On the Probability of Detecting Picoseismicity, Bull. Seismol. Soc. Am. 101, no. 6, 2579–2591, doi 10.1785/0120110017.

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Naoi, M., M. Nakatani, Y. Yabe, G. Kwiatek, T. Igarashi, and K. Plenkers (2011). Twenty thousand aftershocks of a very small (M2) earthquake and their relations to the mainshock rupture and geological structures, Bull. Seismol. Soc. Am. 101, no. 5, 2399–2407, doi 10.1785/0120100346.

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Kwiatek, G., K. Plenkers, M. Nakatani, Y. Yabe, G. Dresen, and J. Group (2010). Frequency-Magnitude Characteristics Down to Magnitude -4.4 for Induced Seismicity Recorded at Mponeng Gold Mine, South Africa, Bull. Seismol. Soc. Am. 100, no. 3, 1167–1173, doi 10.1785/0120090277.

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