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CO<sub>2</sub>-driven biosurfactant synthesis by bacteria within CCUS. [PDF]

open access: yesAppl Microbiol Biotechnol
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28th September 2018 Mw 7.5 Sulawesi Supershear Earthquake, Indonesia: Ground effects and macroseismic intensity estimation using ESI-2007 scale

Engineering Geology, 2023
The 28th September 2018 Sulawesi Supershear earthquake (MW 7.5) was one of the deadliest earthquakes in the recent history of Indonesia causing ~4000 causalities. The earthquake caused a ~ 177 km long surface rupture along the Palu-Karo fault. Apart from surface rupture, the earthquake caused extensive earthquake environmental effects (EEEs) around the
Sambit Prasanajit Naik a   +12 more
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Macroseismic intensity assessment of 1885 Baramulla Earthquake of northwestern Kashmir Himalaya, using the Environmental Seismic Intensity scale (ESI 2007)

Quaternary International, 2014
Abstract Kashmir has a long written history of 5000 years, which provides a sketchy picture of historical earthquakes. In all, we collated details of 16 earthquakes from the historical scribes. Most of the earthquakes had their epicenters outside the Kashmir Valley.
Bashir Ahmad, Hamid Sana, Akhtar Alam
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Uncertainty in intensity assignment and attenuation relationships: How seismic hazard maps can benefit from the implementation of the Environmental Seismic Intensity scale (ESI 2007)

Quaternary International, 2011
Fault slip-rates are of decisive importance for seismic hazard assessment. However, sensitivity analysis in geological fault slip-rate seismic hazard maps demonstrates that the uncertainty in the attenuation relationships is much higher than the implied uncertainty in slip-rates, so that even if more accurate slip-rate estimation is achieved, it would ...
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Earthquake-Induced Rockfalls Caused by 1998 Mw5.6 Earthquake in Krn Mountains (NW Slovenia) and ESI 2007 Intensity Scale

2017
The 12 April 1998 Mw5.6 Krn Mountains earthquake with a maximum intensity of VII-VIII on the EMS-98 scale caused extensive environmental effects in the Julian Alps. The application of intensity scales based mainly on damage to buildings was limited in the epicentral area, because it is a high mountain area and thus very sparsely populated. On the other
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