Volcanism in the Baikal rift: 40 years of active-versus-passive model discussion
AV Ivanov, EI Demonterova, H He, AB Perepelov… - Earth-Science …, 2015 - Elsevier
In this review we focus on the volcanism, that occurred in Transbaikalia, Siberia after the
closure of the Mongolia-Okhotsk Ocean. The closure happened in the Early Jurassic. After …
closure of the Mongolia-Okhotsk Ocean. The closure happened in the Early Jurassic. After …
Imaging the lithosphere and upper mantle: Where we are at and where we are going
In recent years, advances on computational power, inversion methods, and laboratory
experimental techniques, as well as the dramatic increase on both quality and quantity of …
experimental techniques, as well as the dramatic increase on both quality and quantity of …
Upper-mantle seismic structure in a region of incipient continental breakup: northern Ethiopian rift
ID Bastow, GW Stuart, JM Kendall… - Geophysical Journal …, 2005 - academic.oup.com
The northern Ethiopian rift forms the third arm of the Red Sea, Gulf of Aden triple junction,
and marks the transition from continental rifting in the East African rift to incipient oceanic …
and marks the transition from continental rifting in the East African rift to incipient oceanic …
Structure and evolution of the Baikal rift: a synthesis
C Petit, J Deverchere - Geochemistry, Geophysics, Geosystems, 2006 - Wiley Online Library
Active continental rifts are spectacular manifestations of the deformation of continents but
are not very numerous at the surface of the Earth. Among them, the Baikal rift has been …
are not very numerous at the surface of the Earth. Among them, the Baikal rift has been …
How old is the Baikal Rift Zone? Insight from apatite fission track thermochronology
Apatite fission track analysis (AFTA) data are used to bring new light on the long‐term and
recent history of the Baikal rift region (Siberia). We describe the evolution of the topography …
recent history of the Baikal rift region (Siberia). We describe the evolution of the topography …
The crustal thickness of West Antarctica
P‐to‐S receiver functions (PRFs) from the Polar Earth Observing Network (POLENET) GPS
and seismic leg of POLENET spanning West Antarctica and the Transantarctic Mountains …
and seismic leg of POLENET spanning West Antarctica and the Transantarctic Mountains …
Joint inversion of potential field data with adaptive unstructured tetrahedral mesh
Inverting potential field data presents a significant challenge due to its ill-posed nature, often
leading to nonunique model solutions. Addressing this, our work focuses on developing a …
leading to nonunique model solutions. Addressing this, our work focuses on developing a …
1.11 crust and lithospheric structure–global crustal structure
WD Mooney - Seismology and Structure of the Earth: Treatise on …, 2010 - books.google.com
366 366 368 369 370 372 372 372 373 373 373 374 375 375 376 379 379 380 380 380
381 384 384 387 388 389 389 389 394 394 395 395 397 398 11.1 challenges in the form of …
381 384 384 387 388 389 389 389 394 394 395 395 397 398 11.1 challenges in the form of …
Continental rifting as a function of lithosphere mantle strength
The role of the uppermost mantle strength in the pattern of lithosphere rifting is investigated
using a thermo-mechanical finite-element code. In the lithosphere, the mantle/crust strength …
using a thermo-mechanical finite-element code. In the lithosphere, the mantle/crust strength …
Complex geological-geophysical 3D model of the crust in the southeastern Fennoscandian Shield: Nature of density layering of the crust and the crust-mantle …
VN Glaznev, MV Mints, OM Muravina… - Геодинамика и …, 2015 - cyberleninka.ru
The complex geophysical 3D model of the Earth's crust and the upper mantle is created for
the Archaean Karelian Craton and the Late Palaeoproterozoic accretionary Svecofennian …
the Archaean Karelian Craton and the Late Palaeoproterozoic accretionary Svecofennian …