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variations in subsidence and by changes in sea level and climate(passive) are influenced bypatterns of sediment accumulation in sedimentary basins
to take excess flow during storm events(passive) are designedOff - line sediment basins
of other rock fragments that were cemented by silicate minerals(passive) are composedsubsequent Clastic sedimentary rocks
Tectonic activity at all of these marginscausesthe formation of sedimentary basins
the potentialto influencethe formation of sedimentary basins
Ongoing erosion and weatheringresultedin sedimentary rocks infilling the basins
factorsinfluencingerosion in the basins
Earthquakescan causeliquefaction of loose sediments
the deformation of genesisresultedfrom sedimentary protoloth metamorphism
erosioncontributessediment to stormwater
to slow water down so sediments can settle(passive) are designedSediment basins
to provide an area for runoff to pool and settle out a portion of the sediment(passive) are designedSediment basins
Subsequent earth movementscauseduplift of the sedimentary basins
t capture site(passive) are designedSediment basins
Subsequent earth movements ... migration of the petroleumcauseduplift of the sedimentary basins
the cratonic collisionresultedin the foreland sedimentary Padbury Basin
Culmination of the cratonic collisionresultedin the foreland sedimentary Padbury Basin
The freezingcausedfracturing of the sediment
to trap silt as it migrates toward the lake and hold it rather than allowing it to flow into the main lake(passive) are designedSediment basins
with detention time(passive) are designedSediment basins
to a sufficient size(passive) should be designedSediment basins
i. You will learnhow to designsediment basins
geographical processescontributeto shaping sedimentary basins
worldwide(passive) have been discoveredSome 600 sedimentary basins
to reduce runoff rates and to remove pollutants(passive) are designedSedimentation basins
the eastern wallis composedof the clastic sedimentary sediments
by gravel , sand and clay(passive) composed byquaternary alluvial sediments
by the extraction of groundwater and natural gas(passive) caused byfloodplain sediment
by strike - slip deformation of the lithosphere(passive) caused bySedimentary basin
of fragments of rock(passive) are composedClastic sediments
rock fragmentscontributingclastic sediments
by gravel , sand and clay(passive) composed byalluvial sediments
the United Statesoriginatedfrom shale basins
streams under surface conditions(passive) are influenced byFluvial sediments
of the shells ( tests , frustules ) of microscopic plankton , both animal ( zooplankton ) and plant ( phytoplankton ) plankton(passive) is composedBiogenic pelagic sediment
Scientistshave discoveredsedimentary basins
the most important propertiesinfluencingthe sedimentary basins
Some common claysoriginatein sedimentary basins
by the degree of slope gradient(passive) was influenced byeroded sediments
to trap and control sedimentare designedto trap and control sediment
the intrabasement reflectionscausingthe intrabasement reflections
to this load in both areascontributedto this load in both areas
from the erosion of older rocksresultfrom the erosion of older rocks
Increased shaking(passive) caused byIncreased shaking
in our timeoriginatedin our time
increased turbiditycan causeincreased turbidity
from different depositional environmentsresultedfrom different depositional environments
of graphitic argillites and greywackescomposedof graphitic argillites and greywackes
from changes in texture or composition during depositionmay resultfrom changes in texture or composition during deposition
gravity lowscausegravity lows
in the Late Jurassicoriginatedin the Late Jurassic
in the Pacific Northwest areadiscoveredin the Pacific Northwest area
of silicaprincipally composedof silica
of unconsolidated sands and gravelscomposed largelyof unconsolidated sands and gravels
of quartz and feldspar crystalsmost commonly composedof quartz and feldspar crystals
to protect water supplies and communitiesdesignedto protect water supplies and communities
in severe damagemay resultin severe damage
from the Pleistocene rocks , which form the nearby mountainsoriginatingfrom the Pleistocene rocks , which form the nearby mountains
mainly of sand and fine gravelscomposingmainly of sand and fine gravels
from the pelagic zoneoriginating exclusivelyfrom the pelagic zone
during Carboniferous - Early Permian riftingoriginatedduring Carboniferous - Early Permian rifting
of broken rocksare ... composedof broken rocks
of diatomites , red beds , fluvial materials and paleosolscomposedof diatomites , red beds , fluvial materials and paleosols
the initial depressioncausingthe initial depression
adjacent areas to subsidecauseadjacent areas to subside
the majority of growth in U.S. hydrocarbon productionhave contributedthe majority of growth in U.S. hydrocarbon production
with a progressively stronger continental influencesettingwith a progressively stronger continental influence
from the uplift of Sumatraoriginatingfrom the uplift of Sumatra
of perfectly consistent layers of rockbeing composedof perfectly consistent layers of rock
over timeresultover time
7 % of the SNR study unitcompose7 % of the SNR study unit
from the interaction between different tectonic platesresultfrom the interaction between different tectonic plates
to Mount Sharpleadingto Mount Sharp