HelioWebRAS, Institute of the Earths Crust, Irkutsk
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I[RAS, Institute of the Earths Crust, Irkutsk]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (18)"]
CA["Linked Collaborating Authors (1)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Relationships Between Seismicity and GPS Determined Velocities in Northeast Asia
- Seismic Process in Active Faults of the Baikal Rift System
- Seismicity and Tectonic Stress Field of the Laptev Sea Shelf
- Why are Low-Ti Basalts of the Siberian Traps Large Igneous Province Similar to Island Arc Basalts?
- Quasi-hydrostatic equation of state of iron above 2 Mbar; implications for the Earth's core
- Upper Mantle Flow Beneath the Hangay Dome, Central Mongolia
- Geochronology and Paleomagnetism of Mafic Igneous Rocks in the Olenek Uplift, Northern Siberia: Implications for Mesoproterozoic Paleogeography
- Mie-Grüneisen-Einstein Equation of State as a Practical High Temperature Pressure Scale
- Earthquake Geology of the Bulnay Fault, Mongolia
- Using speleothem growth periods to constrain Quaternary evolution of Siberian permafrost
- Dipole low at the Permo-Triassic boundary? New paleomagnetic data from the central Siberian Traps
- Where was Siberia in Mid Paleozoic? New paleomagnetic evidence
- 1,350,000 Year History of Siberian Permafrost Based on U-Pb Chronology of Speleothems
- Can silicon isotopes be used to assess anthropogenic impacts and nutrient utilisation in Lake Baikal, Siberia?
- Contemporary limnological and sedimentary analyses to investigate anthropogenic changes in nutrient fluxes at Lake Baikal, Siberia
- The Neogene de-greening of Central Asia
- Geodynamics of Modern Structures and Seismotectonics of the Russian Northeast
- Fluids migration through permafrost and the pool of greenhouse gases in frozen soils