Active Margins
Active Margins is a tectonic boundary characterized by the convergence or divergence of lithospheric plates, distinguished from passive margins by frequent seismic and volcanic activity resulting from ongoing plate interactions.
149
Publications
20.4K
Citations
447
Authors
224
Institutions
Publications per year
2017–2026
35
Parents
149
Tectonic models for accretion of the Central Asian Orogenic Belt
Brian F. Windley, D. V. Alexeiev, Wenjiao Xiao et al. · Journal of the Geological Society · 2006 · 3.4K citations · Full text
1–5 of 149
447
8
h-index
4
h-index
3
h-index
2
h-index
2
h-index
1–5 of 447
224
ETH Zurich
Zurich, Switzerland
10 h-index
15 publications
1.3K citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
21 publications
924 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
12 publications
9.7K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
5 h-index
8 publications
645 citations
Institute of Geology and Geophysics
Beijing, China
4 h-index
10 publications
7.6K citations

National Taiwan University
Taipei, Taiwan
4 h-index
10 publications
358 citations

University of Oslo
Oslo, Norway
4 h-index
9 publications
288 citations
Russian Academy of Sciences
Moscow, Russia
4 h-index
7 publications
3.6K citations
1–8 of 224
9 publications · 3.5K citations
9
h-index
9 publications · 751 citations
9
h-index
JGS · 7 publications · 3.9K citations
7
h-index
JGR · 7 publications · 590 citations
7
h-index
5 publications · 160 citations
5
h-index
1–5