Karst Subsidence
Karst Subsidence is a geological hazard characterized by the sudden or gradual collapse of the land surface due to the dissolution of underlying soluble bedrock, typically composed of limestone, gypsum, or salt, resulting in the formation of sinkholes or depressions.
280
Publications
10.9K
Citations
777
Authors
343
Institutions
Publications per year
2017–2026
69
Parents
280
1–5 of 280
777
14
h-index
7
h-index
7
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6
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1–5 of 777
343
Universidad de Zaragoza
Zaragoza, Spain
18 h-index
72 publications
3.5K citations

Chinese Academy of Sciences
Beijing, China
9 h-index
22 publications
1.1K citations
Hebrew University of Jerusalem
Jerusalem, Israel
6 h-index
9 publications
270 citations
Institute of Geochemistry
Guiyang, China
5 h-index
11 publications
484 citations
University of Chinese Academy of Sciences
Beijing, China
5 h-index
7 publications
381 citations

Sorbonne Université
Paris, France
5 h-index
9 publications
1.6K citations
National Research Council
Rome, Italy
5 h-index
8 publications
532 citations
Sinopec (China)
Beijing, China
5 h-index
9 publications
189 citations
1–8 of 343
24 publications · 1.2K citations
20
h-index
25 publications · 876 citations
20
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17 publications · 468 citations
13
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14 publications · 587 citations
13
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11 publications · 516 citations
11
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1–5