The development of quartz-dolomite hydrothermal vein complexes synchronous with slip along the Zuccale low-angle normal fault, Italy: evidence for overpressure, weakening and paleoseismicity

    flowchart
    W[2011AGUFM.T33E2456H]
    LA["Linked Authors (0)"]
    LI["Linked Institutions (2)"]
    W== author ==>LA
    W== affil ==>LI
    click LA "#linked-authors"
    click LI "#linked-institutions"
Graph neighborhood for 'The development of quartz-dolomite hydrothermal vein complexes synchronous with slip along the Zuccale low-angle normal fault, Italy: evidence for overpressure, weakening and paleoseismicity'. Click aggregate nodes to navigate.
ADS bibcode
2011AGUFM.T33E2456H
year
2011
Listed Authors
Holdsworth, R. E.
Smith, S.
Lloyd, G.
Dempsey, E. D.
Listed Institutions
Dept Earth Sciences, Univ Durham, Durham, United Kingdom;
Seismology and Tectonophysics Section, INGV, Rome, Italy;
School of Earth & Environment, University of Leeds, Leeds, United Kingdom;
Dept Earth Sciences, Univ Durham, Durham, United Kingdom;

Linked Authors [?]

Linked Institutions