2004
DOI: 10.1016/j.soildyn.2003.10.001
|View full text |Cite
|
Sign up to set email alerts
|

Rockburst induced ground motion—a comparative study

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

2
33
0
2

Year Published

2011
2011
2020
2020

Publication Types

Select...
5
3
1

Relationship

1
8

Authors

Journals

citations
Cited by 52 publications
(37 citation statements)
references
References 6 publications
2
33
0
2
Order By: Relevance
“…Parametrem, który wyraźnie odróżnia wstrząsy górnicze od trzęsień ziemi jest czas trwania intensywnej fazy przebiegów drgań [13,14]. W przypadku trzęsień ziemi ten czas wynosi 20 s i więcej, a w przypadku wstrząsów górni-czych 0,5 -2,5 s.…”
Section: Fale Powierzchniowe Epicentrumunclassified
“…Parametrem, który wyraźnie odróżnia wstrząsy górnicze od trzęsień ziemi jest czas trwania intensywnej fazy przebiegów drgań [13,14]. W przypadku trzęsień ziemi ten czas wynosi 20 s i więcej, a w przypadku wstrząsów górni-czych 0,5 -2,5 s.…”
Section: Fale Powierzchniowe Epicentrumunclassified
“…In a paper by Zembaty (2004) ground motions from rockbursts from a copper mining basin in Western Poland were analyzed in detail to define differences as well as similarities to earthquake records motions. Following the Johnston (1992) paper two, characteristic types of rockbursts were identified with respect to their surface records:…”
Section: Rockbursts and Measures Of Their Intensity On The Ground Surmentioning
confidence: 99%
“…When it comes to rockbursts the role of PGV still is important, particularly for the type I rockbursts (Zembaty 2004;Johnston 1992). Also for the type II rockbursts or natural earthquakes PGV can be employed as a measure of cracking damage for PGVs for dominant frequencies of 2-3 Hz and above.…”
Section: Rockbursts and Measures Of Their Intensity On The Ground Surmentioning
confidence: 99%
“…In Poland, there are regions of large paraseismic activity caused by underground mining exploitation. Among particularly active regions are: the Upper Silesian Coal Basin (USCB) (Tatara 2012); the LegnickoGłogowski Copper Region (LGCR) (Pytel 2003;Tatara and Pachla 2010a, b ;Zembaty 2004Zembaty , 2011Tatara 2012;Kuźniar and Tatara 2015;Maciag et al 2016) and the Bełcha-towski Brown Coal Region (BBCR) (Tatara and Pachla 2010a, b;Tatara 2012). In many cases, the structures situated in these areas were neither designed for nor verified for additional seis-mic loads resulting from buildings vibrations.…”
Section: Introductionmentioning
confidence: 99%