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Transition between oceanic and continental lithosphere that is not an active plate margin
A passive margin is the transition between oceanic and continental lithosphere that is not an active plate margin. A passive margin forms by sedimentation
Passive_margin
Zone of the ocean floor
outermost zone of the continental margin. There are two types of continental margins: active and passive margins. Active margins are typically associated with
Continental_margin
Large sedimentary basin in the US
marine sedimentation onto the ancestral Tobosa Basin characterized the passive margin, shallow marine environment. The Tobosa Basin also contains basement
Permian_Basin_(North_America)
Regions of long-term subsidence creating space for infilling by sediments
form a passive margin. In this case the sedimentary rocks of the rift basin phase are overlain by those rocks deposited during the passive margin phase
Sedimentary_basin
Form of transitional crust
Volcanic passive margins (VPM) and non-volcanic passive margins are the two forms of transitional crust that lie beneath passive continental margins that
Volcanic_passive_margin
Geology of the area in California and Nevada
straits. A passive margin developed on the edges of these new seas in the Death Valley region. Carbonate banks formed on this part of the two margins only to
Geology of the Death Valley area
Geology_of_the_Death_Valley_area
Atlantic Coast turned from an active margin into a passive one. Terranes were no longer accreted onto the margin; instead, sediment eroded off the Appalachians
Geology_of_North_America
Geological fold structures in the Middle East and northeast Africa
by extensional tectonics, was associated with the development of a passive margin in northern Africa as the Neotethys Ocean was formed. The second, dominated
Syrian_Arc
Geological process of stretching planet crust
antiformal closures and these are known as metamorphic core complexes. Passive margins above a weak layer develop a specific set of extensional structures
Extensional_tectonics
Rockall–Porcupine margin or Irish-Scottish margin is part of the continental margin of Northwestern Europe, lying to the west of Ireland and Scotland. The margin is
Rockall–Porcupine_margin
Non-volcanic passive margins (NVPM) constitute one end member of the transitional crustal types that lie beneath passive continental margins; the other
Non-volcanic_passive_margins
Fifth period of the Paleozoic Era
the passive margin of northeastern Laurussia (Baltica craton). The suture zone between the former island arc complex and the continental margin formed
Carboniferous
First geological period of the Paleozoic Era
convergent margin. Along the then western margin, Late Neoproterozoic to early Cambrian rifting was followed by the development of a passive margin. To the
Cambrian
Coastal and oceanic landform
of the deep ocean basin proper, but the flooded margins of the continent. Passive continental margins such as most of the Atlantic coasts have wide and
Continental_shelf
Geological processes that underlie the formation of mountains
no widely accepted geophysical model that explains elevated passive continental margins such as the Scandinavian Mountains, eastern Greenland, the Brazilian
Mountain_formation
Landmass comprising more than one continental core, or craton
where passive margins form. The edges of these continents may rift. At this point, seafloor spreading becomes the driving force. Passive margins are therefore
Supercontinent
Large geographical region identified by convention
comprising the continental cratons. The margins of geologic continents are either active or passive. An active margin is characterised by mountain building
Continent
Geological process at tectonic plate boundaries
passive margin. Some passive margins have up to 10 km (6.2 mi) of sedimentary and volcanic rocks covering the continental crust. As a passive margin is
Subduction
Late-Proterozoic to early-Palaeozoic continent
Mesoproterozoic sediments. The margin became a passive margin facing the Ural Ocean in the Cambrian–Ordovician. The eastern margin stretches south through the
Baltica
Foreland basin in Venezuela
South American Plate developed into a passive margin with the Proto-Caribbean Seaway. This stable passive margin allowed for thermal subsidence to occur
Maracaibo_Basin
Bay on the east coast of North America
drifting, and inversion on the passive margin of central eastern North America: an analog for other passive margins". AAPG Bulletin. 82 (5 A): 817–835
Bay_of_Fundy
Sinking of the Earth's crust on a large scale
subsidence on a large scale in a variety of environments, including passive margins, aulacogens, fore-arc basins, foreland basins, intercontinental basins
Tectonic_subsidence
Mountain range in eastern North America
continental margin coincident with the initiation of subduction. Thrust faulting uplifted and warped older sedimentary rock laid down on the passive margin. As
Appalachian_Mountains
Large basin containing the Rub' al Khali desert
halite deposition. This tectonic regime gradually transitioned into a passive margin setting with the opening of the Neo-Tethys in the Early Triassic. During
Rub'_al_Khali_Basin
Severe glaciation during the Paleoproterozoic era
have occurred within a rift basin that evolved into a largely marine passive margin setting. The glacial diamictite deposits within the Huronian are on
Huronian_glaciation
Oilfield in India
Krishna Godavari Basin is a peri-cratonic passive margin basin in India. It is spread across more than 50,000 square kilometres in the Krishna River and
Krishna_Godavari_Basin
Geologic formation in Colombia
subdivided into six phases. The basin started as a passive margin in the Paleozoic, followed by a compressive margin in the Late Permian to Triassic, a phase of
Cesar-Ranchería_Basin
Desert in the southwestern United States
Mojave was again likely submerged under a greater sea. The passive margin switched to active margin in the early-to-mid Mesozoic when the Farallon Plate under
Mojave_Desert
models: Passive continental margin model Crystalline axis model Accreted terrane model Carboniferous-extension model This model is a single margin model
Pre-collisional_Himalaya
Process of evolution of Earth's crust
strike-slip faults, in back-arc basins, and on the continental end of passive margin sequences where a detachment layer is present. Thrust tectonics is associated
Tectonics
First period of the Mesozoic Era
the thinned crust of Greater India, the northern margin of which supplied sediments to the passive margin. The counterclockwise rotation of Pangea precipitated
Triassic
Geological formation in Italy and Switzerland
Formation, and was probably a shallow water succession, developed on the passive margin of the westernmost Southern Alps. It is known due to the exquisite preservation
Moltrasio_Formation
Fourth period of the Paleozoic Era
Gondwana was mostly a passive margin, hosting extensive marine deposits in areas such as northwest Africa and Tibet. The eastern margin, though warmer than
Devonian
"megamullions". Passive margins form during the break-up of existing continental masses as the product of progressive rifting. On some margins, there is very
Exhumed_mantle
Sedimentary basin in Australia
offshore in water depths ranging from 50-3,000 meters. Otway represents a passive margin rift basin and is one of a series of basins located along the Australian
Otway_Basin
Mountain range in Oman and the UAE
the modern convergence of the Australian passive margin under Eurasian oceanic crust, Arabian passive margin sediments became highly deformed and shortened
Hajar_Mountains
Geologic description of the Appalachian Mountains
continental margin, coincident with the initiation of subduction. Thrust faulting uplifted and warped older sedimentary rock laid down on the passive margin. As
Geology_of_the_Appalachians
First period of the Cenozoic Era
development of the Dinarides, Hellenides and Tauride mountain chains as the passive margin sediments of Adria were scrapped off onto the Eurasia crust during subduction
Paleogene
Fields with over 500 million barrels of recoverable oil or gas equivalent
fields exist in two characteristic tectonic settings—passive margin and rift environments. Passive margins are found along the edges of major ocean basins
Giant_oil_and_gas_fields
African submarine canyon at the end of the Congo River
view of the interaction between a giant submarine fan and a mature passive margin (ZaiAngo project)". Tectonophysics. 470 (1): 42–56. Bibcode:2009Tectp
Congo_Canyon
Repeated joining and separation of Earth's continents
sediment depths, emplacement of large igneous provinces, and the effect of passive margin extension. Of these, oceanic crust age, and marine sediment depths seem
Supercontinent_cycle
platforms and passive margin basins existed in South Australia – – formed in the foreland of the Delamerian Orogeny. Western Australian passive margin basins
Geology_of_Australia
(COTZ) is the boundary between continental crust and oceanic crust on a passive margin or the zone of transition between these two crustal types. The identification
Continent-ocean_boundary
Mountain range in Finland, Norway, and Sweden
geologists. Geologically, the Scandinavian Mountains are an elevated, passive continental margin similar to the mountains and plateaux found on the opposite side
Scandinavian_Mountains
Coastal sedimentary basin of Brazil
Campos Basin contains the Paraiba do Sul River delta. The South Atlantic margin developed on Archean stable cratons consisting of hard and resistant rocks
Campos_Basin
Concept in structural geology
on strike-slip faults and as part of detached fault systems on some passive margins. In areas of thrust tectonics, two main processes are recognized: thin-skinned
Thrust_tectonics
Geology and geomorphology of a national park in New Zealand
Overlying the arc-related sequence is a Late Cambrian to Early Devonian passive margin succession of clastic and carbonate sedimentary rocks. The Tākaka terrane
Geology and geomorphology of Kahurangi National Park
Geology_and_geomorphology_of_Kahurangi_National_Park
Metamorphic or igneous rocks below a sedimentary platform or cover
divergent to passive margin tectonics along the Appalachian Mountains. After seafloor spreading began in the Early Jurassic, the margin (the future east
Basement_(geology)
Oil field in Venezuela
Maracaibo Basin. Thermal subsidence and tectonic quiescence of the passive margin led to sediment accumulation and the absence of deformation of the basin
Bolivar_Coastal_Fields
North American geological structure
earthquake to have occurred along the passive margin of North America and possibly the largest passive-margin earthquake worldwide. Coincidentally, it
Canadian_Arctic_Rift_System
the Rodinia supercontinent and the formation of the Iapetus Ocean. Passive margin sequences are preserved within the lowermost allochthon and parautochthon
Geology_of_Norway
Offshore oil field in Vietnam
inspection of the seismic profile of the area shows faulted basement passive margin which is sealed by an onlapping sedimentary sequence. It is plausible
Bạch_Hổ_oil_field
Sardinia Margin is a fault-bounded passive margin located northwest of the Vavilov Basin. Seismic reflection surveys across the Upper Sardinia Margin exhibit
Tyrrhenian_Basin
Steep-sided valley cut into the seabed of the continental slope
common on the steep slopes found on active margins compared to those on the gentler slopes found on passive margins. They show erosion through all substrates
Submarine_canyon
Batholith in the Sierra Nevada mountain range, United States
metamorphosed. The "host rocks" include passive margin sequence units, deep water sediments, and shallow-water passive margin units. There are several locations
Sierra_Nevada_Batholith
Origins and structure of the Himalayan Mountain range
was accommodated by thrusting and folding of the sediments of the passive Indian margin together with the deformation of the Tibetan crust. Even though
Geology_of_the_Himalayas
Atlantic fragment of continental crust
Atlantic margin (Aegir Ridge in this area), the Jan Mayen Microcontinent formed part of the passive margin developed along the East Greenland margin. Towards
Jan_Mayen_Microcontinent
Type of quartzite rock
to possibly define a large sedimentary wedge that once covered the passive margin on the then-southern side of the North American craton. In human history
Sioux_Quartzite
Neoproterozoic to Cretaceous landmass
northern margin remained a mostly passive margin throughout the Paleozoic. The Early Permian opening of the Neo-Tethys Ocean along this margin produced
Gondwana
Sedimentary basin off Newfoundland
deformed strata were deposited on the newly established passive margin. The current passive margin conditions were established when the last rifted border
Jeanne_d'Arc_Basin
Precambrian craton that with four others makes up the modern continent of Africa
break-up. During the Neoproterozoic, Central Congo or Bas-Congo became a passive margin on which was deposited 4,000 m (13,000 ft) sediments. At the end of
Congo_Craton
Major geological province in Australia
a rift basin. After about 725 Ma, deposition continued in a mostly passive margin setting along the western edge of the Palaeo-Pacific Ocean, with renewed
Adelaide_Superbasin
Orientation of a geologic feature
plate interactions Mélange Mountain formation Nappe Obduction Orogeny Passive margin Plate tectonics Pull-apart basin Rift valley Rift Saddle Strike-slip
Strike_and_dip
Geological strata
nature and develop as a response to extensional collapse of a passive continental margin (i.e. Niger Delta, Mississippi Delta). Their main feature is that
Rollover_anticlines
over huge areas, up to 107 km2 in extent and have been described from passive margins around the world. Most examples have been identified using 3D seismic
Polygonal_fault
portion of Patagonia was separated from Gondwana, and the resulting passive margin that formed was a site of extensive sedimentation throughout the early-middle
Tectonic evolution of Patagonia
Tectonic_evolution_of_Patagonia
Sedimentary rock deposit associated with the formation of mountain chains
to molasse transition in peripheral foreland basins: the role of the passive margin versus slab breakoff" Geology 25(12): pp. 1123–1126, doi: 10
Molasse
Silt deposition landform at the mouth of a river
along passive continental margins. This phenomenon is due mainly to three factors: topography, basin area, and basin elevation. Topography along passive margins
River_delta
Supposed tectonic microplate containing the Greenland craton
Geller, R.J., Wang, S.-C. & Kroeger, G.C. (1979). "Earthquakes along the passive margin of eastern Canada". Geophysical Research Letters. 6 (7). Geophys. Res
Greenland_plate
Geologic region in Eastern Canada
represented by the accreted arc on preexisting Laurentia caused magmatism. A passive margin that accumulated sediment formed due to lack of tectonic activity. The
Grenville_Province
Terrane in the northern Appalachians which broke off the supercontinent Gondwana
Early Palaeozoic siliciclastic rocks of the Gander Zone, the eastern passive margin of the Iapetus Ocean, now found in Newfoundland, New Brunswick, and
Ganderia
Topics referred to by the same term
Continent-ocean boundary, the boundary between oceanic and continental crust on a passive margin Contingency Operating Base, a US military term, a forward operating
Cob
The Exmouth Plateau is an elongate northeast striking extensional passive margin located in the Indian Ocean roughly 3,000 meters offshore from western
Exmouth_Plateau
Long, narrow crack opening on a planetary surface
plate interactions Mélange Mountain formation Nappe Obduction Orogeny Passive margin Plate tectonics Pull-apart basin Rift valley Rift Saddle Strike-slip
Fissure
Old and stable part of the continental lithosphere
geologically recent rifting events have separated cratons and created passive margins along their edges. Cratons are composed of ancient crystalline basement
Craton
Thrust belt
epicontinental sea separating the European foreland from the northern passive margin of the Alpine Tethys. They are overlain, particularly in the south,
Geology_of_the_Jura_Massif
Tectonic plate including Southeast Asia
subducting under oceanic. However, it then transitioned to continental passive margin subducting under oceanic plate. This rare phenomenon continues due to
Sunda_plate
Marginal sea of the Atlantic Ocean
stretches of sandy beach. The Gulf of Mexico is an excellent example of a passive margin. The continental shelf is quite wide at most points along the coast
Gulf_of_Mexico
Earthquake that struck Greenland and the Northwest Territories (now Nunavut), Canada
Nunavut. The event is the largest recorded earthquake to strike the passive margin of North America and is the largest north of the Arctic Circle. It is
1933_Baffin_Bay_earthquake
Geological feature in the Atlantic Ocean
Consequently, this area is a rare case of a passive margin slowly being transformed into an active margin. The extension of this subduction system, known
Azores–Gibraltar transform fault
Azores–Gibraltar_transform_fault
Geology of salt structures
from neighbouring piercements to form canopies.[citation needed] On passive margins where salt is present, such as the Gulf of Mexico, salt tectonics largely
Salt_tectonics
calcareous black and gray shales. It was deposited in a shallow marine passive margin setting. It is conformably overlain by the Alacaagzi Formation, and
Zonguldak_basin
Landform created by the action of glaciers
Atle; Ottesen, Dag (2013). "Selective glacial erosion on the Norwegian passive margin". Geology. 41 (12): 1203–1206. Bibcode:2013Geo....41.1203H. doi:10.1130/g34806
Glacial_landform
scales, and at numerous locations on Earth, from rhyolite lava flows to passive margins. Additionally, gravity spreading is likely to have occurred on both
Gravity_spreading
Band in the Earth's crust from East Antarctica to the Arabian-Nubian Shield
Tanzania include rift sediments and passive margin metasediments from the early Neoproterozoic continental margin. They also include older crustal material
Mozambique_Belt
Hypothesized Neoproterozoic supercontinent
diversification. Bond, Nickeson & Kominz 1984 found Neoproterozoic passive margin sequences worldwide—the first indication of a Late Neoproterozoic supercontinent
Pannotia
Emergent coastal landform
such as subduction on the Pacific coasts of South and North America, passive margin of the Atlantic coast of South America, collision context on the Pacific
Raised_beach
Atlantic coastal region of the United States
The East Coast, with the exception of Eastern Maine, is a low relief, passive margin coast. It has been shaped by the Pleistocene glaciation in the far northern
East Coast of the United States
East_Coast_of_the_United_States
Island of Indonesia
consequence of the subduction of the Scott Plateau of the Australian passive margin. More work is needed to understand the crustal and tectonic mechanisms
Rote_Island
Mississippian to Jurassic a carbonate ramp built out to the south on the passive margin of the Arctic Alaskan Plate. The Arctic Alaskan Plate was then rifted
Alaska_North_Slope_basin
once per 670 years". The Atlantic continental margin of the Northeastern United States is a passive margin. The seismicity of the northeast is generally
Seismicity of the New York City area
Seismicity_of_the_New_York_City_area
Highest mountain in Namibia
Cretaceous Brandberg and Okenyenya igneous complexes on Namibia's Atlantic passive margin". Tectonics. 24 (3): TC3006. Bibcode:2005Tecto..24.3006R. doi:10.1029/2004TC001688
Brandberg_Mountain
Examples of such basin classifications include intracratonic, rift, passive margin, strike-slip, forearc, backarc-marginal sea, fold and thrust belt, and
Sedimentary_basin_analysis
Uninhabited islet in the North Atlantic Ocean
tectonostratigraphy of the Rockall Plateau, Atlantic margin of NW Britain: Linking early spreading tectonics and passive margin response". Marine and Petroleum Geology
Rockall
Series of mountain ranges along the Pacific coast of North America
group of Canada. A rupture in Rodinia 750 million years ago formed a passive margin in the eastern Pacific Northwest. The breakup of Pangea 200 million
Pacific_Coast_Ranges
Swiss geologist and academic
Mosar presented a structural model for the Scandinavian North Atlantic passive margin, highlighting the asymmetric crustal extension between Greenland and
Jon_Mosar
Oil field in Nigeria
formed as the result of long-term progradation onto the Atlantic Ocean passive margin. They are distinguished from one another on the basis of their sand-to-shale
Delta_Field_(Niger_Delta)
Large geological structure
grouped in two regional dike swarms running oblique to the northern passive margin of the Barents Sea: the Franz Josef Land and Svalbard dike swarms, respectively
Barents_Sea_dike_swarm
Spatial entity with common geologic attributes
Extended crust Continental crust thinned due to extensional strain Passive margin Rift Basin and Range Province Northern Cordilleran Volcanic Province
Geologic_province
Rock overlying a less resistant type
traps for hydrocarbons and shaping the seafloor topography. The Gulf's passive margin setting, with thick sediment accumulation, promotes widespread salt
Caprock
PASSIVE MARGIN
PASSIVE MARGIN
Biblical
passage; leap; step; the passover
Girl/Female
Russian
Abbreviation of Natasha - the Russian form of the English Natalie 'Born at Christmas.
Girl/Female
Indian, Telugu
Unexpected; Massive
Female
English
Pet form of English Cass, CASSIE means "she who entangles men."
Girl/Female
English American
Abbreviation of Cassandra. Unheeded prophetess. In Homer's 'The Iliad' Cassandra's prediction of...
Girl/Female
American, Australian, British, English
Girl; A Little Lass
Girl/Female
Tamil
Passion
Surname or Lastname
English
English : topographic name for someone who lived in a narrow lane or passage, Middle English passage.
Boy/Male
Muslim
Passion
Boy/Male
Tamil
Passion
Girl/Female
English American Greek
Unheeded prophetess. A , Cassandra, or Catherine. Cassandra was a Trojan prophetess, daughter of...
Girl/Female
Biblical
Passage, leap, step, the passover.
Girl/Female
English American
Girl.
Boy/Male
Hindu
Passion
Boy/Male
Tamil
Passage
Girl/Female
American, British, English, Greek
Clever; Unheeded Prophetess; Abbreviation of Cassandra; From Cassandra; She who Entangles Men
Surname or Lastname
English
English : variant spelling of Pass.French : possibly a nickname from passe ‘sparrow’.
Boy/Male
Hindu, Indian, Iranian, Russian
A Massive
Boy/Male
Indian
Passion
Girl/Female
Australian, Russian
Born at Christmas; The Russian Form of the English Natalie; Abbreviation of Natasha
PASSIVE MARGIN
PASSIVE MARGIN
Girl/Female
Indian, Modern
Softness
Boy/Male
Irish
Owns the fields.
Boy/Male
Indian
Decent, Honest and modest, Faithful to God, Name of a Khalifah
Boy/Male
Tamil
Jambavatpreeti | ஜமà¯à®ªà®µà®¤à®ªà¯à®°à¯€à®¤à®¿
Vardhana winner of jambavans Love
Surname or Lastname
English (mainly Cambridgeshire)
English (mainly Cambridgeshire) : habitational name from a place in Lincolnshire called Panton, from Old English pamp ‘hill’, ‘ridge’ or panne ‘pan’ + tūn ‘enclosure’, ‘settlement’.
Surname or Lastname
English
English : variant of Franey.
Boy/Male
Indian, Punjabi, Sikh
Three-eyed
Boy/Male
Hindu
Lord Muruga
Girl/Female
Assamese, Celebrity, Gujarati, Hindu, Indian, Kannada, Malayalam, Marathi, Mythological, Sanskrit, Sindhi, Telugu, Traditional
Fish Eyes; A Daughter of Kubera; Goddess Parvati
Surname or Lastname
Austrian and Swiss German
Austrian and Swiss German : a variant spelling of Hänni, see Hanni.English : variant spelling of Hanney.
PASSIVE MARGIN
PASSIVE MARGIN
PASSIVE MARGIN
PASSIVE MARGIN
PASSIVE MARGIN
adv.
As a passive verb; in the passive voice.
a.
Alt. of Passee
v. i.
To suffer pain or sorrow; to experience a passion; to be extremely agitated.
n.
The sacrifice offered at the feast of the passover; the paschal lamb.
n.
A passing or going through; passage.
n.
The state of being acted upon; subjection to an external agent or influence; a passive condition; -- opposed to action.
v. i.
The act of passing; transit from one place to another; movement from point to point; a going by, over, across, or through; as, the passage of a man or a carriage; the passage of a ship or a bird; the passage of light; the passage of fluids through the pores or channels of the body.
a.
In mass; not necessarily without a crystalline structure, but having no regular form; as, a mineral occurs massive.
adv.
In a passive manner; inertly; unresistingly.
a.
Pressing; urgent; also, oppressive; as, pressive taxation.
a.
Relating to the act of passing or going; going by, beyond, through, or away; departing.
a.
Receiving or enduring without either active sympathy or active resistance; without emotion or excitement; patient; not opposing; unresisting; as, passive obedience; passive submission.
v. i.
Price paid for the liberty to pass; fare; as, to pay one's passage.
a.
Inactive; inert; not showing strong affinity; as, red phosphorus is comparatively passive.
a.
Not active, but acted upon; suffering or receiving impressions or influences; as, they were passive spectators, not actors in the scene.
v. i.
A pass or en encounter; as, a passage at arms.
n.
Passion week. See Passion week, below.
adv.
Exceedingly; excessively; surpassingly; as, passing fair; passing strange.
n.
Specially sent; intended or prepared to be sent; as, a letter missive.
a.
Expressing or suggesting thoughtfulness with sadness; as, pensive numbers.