gptkbp:instance_of
|
gptkb:cave
|
gptkbp:advances
|
contributed to
|
gptkbp:collaboration
|
gptkb:Soviet_Union
|
gptkbp:collaborations
|
international
multidisciplinary
formed
|
gptkbp:collection
|
extensive
|
gptkbp:community
|
recognized
|
gptkbp:completed
|
gptkb:1994
|
gptkbp:conservation
|
conducted
|
gptkbp:core_drilling
|
technique used
|
gptkbp:core_samples
|
obtained
|
gptkbp:country
|
gptkb:Russia
|
gptkbp:defunct
|
gptkb:1992
|
gptkbp:depth
|
gptkb:Set
12262 meters
|
gptkbp:discovery
|
notable
fossilized microorganisms
|
gptkbp:drilling_challenges
|
encountered
|
gptkbp:drilling_duration
|
24 years
|
gptkbp:drilling_method
|
rotary drilling
|
gptkbp:funding
|
gptkb:Soviet_Union
governmental
|
gptkbp:geological_features
|
provided
|
gptkbp:geological_formation
|
conducted
pioneering
investigated
|
gptkbp:geophysical_studies
|
conducted
|
gptkbp:geothermal_gradient
|
high
|
gptkbp:has_implications_for
|
far-reaching
|
gptkbp:historical_legacy
|
important
enduring
|
https://www.w3.org/2000/01/rdf-schema#label
|
Kola Superdeep Borehole
|
gptkbp:impact
|
gptkb:significant
|
gptkbp:impact_on_geology
|
influenced research
|
gptkbp:initial_depth_goal
|
15000 meters
|
gptkbp:is_explored_in
|
ongoing interest
deep Earth
|
gptkbp:location
|
gptkb:Kola_Peninsula
|
gptkbp:notable_feature
|
ultra-deep drilling
|
gptkbp:notable_work
|
geological history
|
gptkbp:purpose
|
gptkb:scientific_research
|
gptkbp:research
|
advanced
innovative
|
gptkbp:research_focus
|
Earth's crust
|
gptkbp:research_importance
|
highly regarded
|
gptkbp:research_institutes
|
gptkb:Russian_Academy_of_Sciences
|
gptkbp:research_output
|
valuable data
|
gptkbp:rock_samples
|
analyzed
|
gptkbp:rock_type_studied
|
gptkb:granite
|
gptkbp:scientific_instruments
|
used
|
gptkbp:scientific_papers
|
published
|
gptkbp:significance
|
deepest artificial point on Earth
|
gptkbp:started_in
|
gptkb:1970
|
gptkbp:temperature_at_depth
|
180 degrees Celsius
|
gptkbp:temperature_increase
|
with depth
|
gptkbp:bfsParent
|
gptkb:Kola_Peninsula
|
gptkbp:bfsLayer
|
4
|