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Topic: Batholith


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 Batholith - Wikipedia, the free encyclopedia
A batholith is a large emplacement of igneous intrusive (also called plutonic) rock that forms from cooled magma deep in the Earth's crust.
Batholiths are almost always made mostly of felsic or intermediate rock-types, such as granite, quartz monzonite, or diorite.
One such batholith is the Sierra Nevada Batholith, which is a continuous granitic formation that forms much of the Sierra Nevadas in California.
en.wikipedia.org /wiki/Batholith   (518 words)

  
 Batholith -- Facts, Info, and Encyclopedia article   (Site not responding. Last check: 2007-11-06)
A batholith is a large emplacement of (Click link for more info and facts about igneous) igneous (Click link for more info and facts about intrusive) intrusive (also called plutonic) rock that forms from cooled (Molten rock in the earth's crust) magma deep in the Earth's (The outer layer of the Earth) crust.
Batholiths are almost always made mostly of (Click link for more info and facts about felsic) felsic or intermediate rock-types, such as (Plutonic igneous rock having visibly crystalline texture; generally composed of feldspar and mica and quartz) granite, (A granular crystalline intrusive rock) diorite or lighter colored forms of (A dark gray volcanic rock) andesite.
An even larger batholith, found predominantly in the mountains of western (A nation in northern North America; the French were the first Europeans to settle in mainland Canada) Canada, extends for 1,800 kilometers and reaches into southeastern (A state in northwestern North America; the 49th state admitted to the union) Alaska.
www.absoluteastronomy.com /encyclopedia/b/ba/batholith.htm   (767 words)

  
 batholith - Hutchinson encyclopedia article about batholith   (Site not responding. Last check: 2007-11-06)
Batholiths form the core of some large mountain ranges like the Sierra Nevada of western North America.
The solidified magma becomes the central axis of a rising mountain range, resulting in the deformation (folding and overthrusting) of rocks on either side.
In the UK, a batholith underlies SW England and is exposed in places to form areas of high ground such as Dartmoor and Land's End.
encyclopedia.farlex.com /batholith   (192 words)

  
 Diapir   (Site not responding. Last check: 2007-11-06)
A batholith is a large emplacement of igneous intrusive (also called plutonic) rockthat forms from cooled magma deep in the earth's crust.
Batholiths are almost always mademostly of felsic or intermediate rock-types such as granite, diorite orlighter colored forms of andesite.
Batholiths exposed at the surface are also subjected to huge pressure differences between their former homes deep in the earthand their new homes at or near the surface.
www.therfcc.org /diapir-166331.html   (495 words)

  
 Batholith   (Site not responding. Last check: 2007-11-06)
A batholith is a large emplacement of igneous intrusive (also called plutonic) rock that from cooled magma deep in the earth's crust.
In spite of their apparent uniformity batholiths in fact structures with complex histories and They are composed of multiple blobs or plutons of magma that traveled toward the from a zone of partial melting at base the earth's crust.
Batholiths exposed at the surface are also to huge pressure differences between their former deep in the earth and their new at or near the surface.
www.freeglossary.com /Plutonic_diapir   (611 words)

  
 batholith on Encyclopedia.com   (Site not responding. Last check: 2007-11-06)
Batholiths usually are granitic (see granite) in composition, have steeply inclined walls, have no visible floors, and commonly extend over areas of thousands of square miles.
Batholiths are formed either as one large mass or many smaller masses at great depths in the earth's crust and are exposed at the surface only after considerable erosion of the overlying mountain mass.
One of the largest single batholiths in North America is the Coast Range batholith of W Canada and Alaska, encompassing an area of about 73,000 sq mi (182,500 sq km).
www.encyclopedia.com /html/b1/batholit.asp   (450 words)

  
 Cooling History of the Okpilak Batholith   (Site not responding. Last check: 2007-11-06)
We investigated the thermal history of the Okpilak batholith, northeastern Brooks Range using the technique of 40Ar/39Ar thermochronology of potassium feldspars.
The Okpilak batholith of the northeastern Brooks Range presents the unusual case of intimate involvement of crystalline rocks in thrusting near the foreland basin of a fold-and-thrust belt.
Samples from four locations in the batholith yielded age spectra indicative of the multidomain behavior of feldspar.
www.gi.alaska.edu /TSRG/Research/TSRG16.html   (257 words)

  
 PROTRACTED END-CALEDONIAN GRANITE MAGMATISM IN IRELAND: FIELD EVIDENCE FROM THE GALWAY BATHOLITH   (Site not responding. Last check: 2007-11-06)
The WNW-ESE long axis of the batholith trends oblique to the pre-emplacement Skird Rocks Fault, considered to be a splay from the continuation of the Southern Uplands Fault of Scotland across Ireland.
Post-dating all the plutons are swarms of microgranite and hypabyssal latite-rhyolite dikes that mostly trend NNE-SSW, perpendicular to the batholith long-axis.
The preserved dike swarms are almost entirely restricted to the western and eastern blocks of the batholith, contrasting with their rarity in the uplifted central block.
gsa.confex.com /gsa/2001NE/finalprogram/abstract_2286.htm   (447 words)

  
 AllRefer.com - batholith (Geology And Oceanography) - Encyclopedia
batholith, enormous mass of intrusive igneous rock, that is, rock made of once-molten material that has solidified below the earth's surface (see rock).
They are commonly associated with lithospheric plate boundaries, where the interactions between plates can produce sufficient heat to melt crustal rocks on a large scale and form batholiths (see plate tectonics).
Important batholiths in the United States include the Idaho batholith, 18,000 sq mi (45,000 sq km), and the Sierra Nevada batholith, 16,000 sq mi (40,000 sq km).
reference.allrefer.com /encyclopedia/B/batholit.html   (282 words)

  
 Mesozoic Plutonism in the Sierra Nevada Batholith
Moore (1962) suggested that the compositional variations in the plutons are representative of magmas generated in a thin sialic layer (west) verses a thick sialic layer (east).
Evidence in the Sierra Nevada batholith as described by Bateman (1988) would seem to suggest that all of these methods of emplacement were active at least in some part.
The gabbroic to granitic intrusives of the Tehachapi Mountains represent the deepest exposures of batholithic cumulates formed at depth of 25-30 km.
www.colorado.edu /GeolSci/Resources/WUSTectonics/SierraBatholith/mesozoic.htm   (2262 words)

  
 batholith --  Encyclopædia Britannica   (Site not responding. Last check: 2007-11-06)
It is commonly composed of coarse-grained rocks (e.g., granite or quartz diorite) with a surface exposure of 100 square km (40 square miles) or larger.
It is abundant in the large batholiths (great masses of igneous rocks mostly deep below the surface) of the world's mountain belts.
These belts are defined by a long linear batholith (large exposed mass of coarse-grained igneous rock) that now extends unbroken to Estados Island in the South Atlantic.
www.britannica.com /eb/article-9013743?tocId=9013743   (429 words)

  
 Bates Geology: John Creasy - White Mountains
Distinctive porphyritic quartz syenite occurs in ring dikes in the western (the Mount Garfield) and the eastern (the Albany) halves of the batholith.
Igneous activity commenced in the western batholith with emplacement of the porphyritic quartz syenite (201 Ma and 193 Ma) and the quartz porphyry (195 Ma) of center W1 and the syenite and trachyte of center W2 (193 Ma).
The porphyritic quartz syenite is similar in appearance across the batholith but occurrences in the eastern and western parts of the batholith are distinguished as the Albany and the Mount Garfield, respectively.
www.bates.edu /acad/depts/geology/jcreasy.WM.html   (3962 words)

  
 Twin Mining Corporation - Geology   (Site not responding. Last check: 2007-11-06)
Exposure of the Idaho batholith is confined to the central region of the state and encompasses approximately 20,000 square miles.
Subsequent post batholithic emplacement throughout the region involved Tertiary dike swarms which trend in a northeast direction and seem to be related to the metallogenic epochs within the Idaho batholith.
The batholith is divided into two distinct lobes, the Bitterroot lobe to the north and the Atlanta lobe, including the Atlanta Project, to the south.
www.twinmining.com /gold_properties/geology.html   (2039 words)

  
 Welcome to Adobe GoLive 5
Batholiths are caused by an enormous mass of intrusive igneous rock ~ rock made of formerly molten material that has solidified below the earth's surface.
Batholiths can be formed either as one large mass or many smaller masses at great depths in the earth's crust.
Important batholiths in the United States include the Idaho batholith, which is 18,000 square miles, and the 16,000 square mile Sierra Nevada batholith.
www.gocornerstore.com /Inventory_files/January%20T%26F/Facts/14F.html   (262 words)

  
 Cornubian Batholith   (Site not responding. Last check: 2007-11-06)
The batholith can be seen at the surface by the exposure of 5 large granite intrusion bodies.
Coarse megacrystic biotite granite is the ‘main’ granite of the batholith, appearing in all the outcrops, and it is estimated to compose 90% of the present exposed area.
The Cornubian batholith was not emplaced as one lump but as several small diapiric plutons over a period of 20 to 30 million years.
www.brookes.ac.uk /geology/8361/1999/simon/cornbath.htm   (1965 words)

  
 SB   (Site not responding. Last check: 2007-11-06)
A Batholith is a large composite intrusion made up of multiple plutons of gabbnoic granitic composition.
Stuart Batholith is a great place to study the processes of arc construction and deformation.
Time of its formation: it is to be believed that this Batholith was formed around the late-cretaceous period, however there is some controversy on the time span of this formation.
academic.evergreen.edu /curricular/MN/stuart_batholith.htm   (146 words)

  
 A PRIMARY LITHOSPHERE SECTION FOR THE SIERRA NEVADA BATHOLITH   (Site not responding. Last check: 2007-11-06)
A primary lithosphere section is reconstructed for the Sierra Nevada batholith based on the convergence of rock types that occurs between the base of its southern oblique crustal section and batholith-related lower crust-mantle xenoliths that were entrained in Miocene lavas erupted through shallow levels of the batholith to the north.
The upper ~35 km of the section is predominately tonalitic to granodioritic batholithic rock with subordinate wallrock screens.
The roof of the batholith is predominately its own silicic volcanic cover, and there is no evidence for the batholith having spread out over a mid-or deep crust regional metamorphic substrate.
gsa.confex.com /gsa/2003AM/finalprogram/abstract_60846.htm   (471 words)

  
 SUB Göttingen - Dissertationen - Becker, Jens Karl: The emplacement of the Chinamora Batholith (Zimbabwe) inferred ...
Becker, Jens Karl: The emplacement of the Chinamora Batholith (Zimbabwe) inferred from field observations, magnetic- and microfabrics
The Chinamora Batholith (Zimbabwe) frequently is stated as a type-locality for the emplacement mechanism of ballooning, however its emplacement mechanism is still the subject of an ongoing discussion.
The Chinamora Batholith is a composite batholith comprising numerous lithologies ranging from dioritic to granitic which may be grouped into the marginal gneissic granites, the equigranular granites and the central porphyritic granite.
webdoc.sub.gwdg.de /diss/2001/becker   (583 words)

  
 Ladakh   (Site not responding. Last check: 2007-11-06)
The Ladakh batholith of northwestern India is one of the most spectacularly exposed continental arc terrains on Earth.
We are initiating a comprehensive study of a portion of this terrain aimed at recovering the timescales of arc magmatism and arc unroofing.
We infer that the Indus molasse thus records a significant proportion of the early unroofing history of the batholith.
www-eaps.mit.edu /research/Hodges/ladakh.html   (325 words)

  
 Title
We propose that the compositional boundary decouples the eastern and western portions of the batholith, and that the eastern portion has thinned in response to regional Miocene extension, or Salton trough rifting, or both.
The Mesozoic Peninsular Ranges batholith is a major component of the southern California crust between the International border and the Transverse Ranges (Fig.
We hypothesize that the steep Moho slope under the eastern Peninsular Ranges batholith is due to the crustal thinning and rifting associated with the opening of the Gulf of California and the Salton trough.
www.seismo.unr.edu /ftp/pub/ichinose/PENINSULAR/peninsular.html   (3913 words)

  
 granite
Most geologists now agree that the batholith owes its existence to the process of tectonic-plate convergence during which melting occurred as a consequence of subduction of oceanic lithosphere (the rigid crust and upper part of the mantle) beneath the margin of the North American continent during Mesozoic time.
The Sierra Nevada batholith is an amalgam of many plutons of varied compositions that intruded the continental crust during subduction.
The batholith as exposed in Yosemite Valley and regions west contains mostly Cretaceous rocks with the rocks in general becoming younger towards the east (Bateman, 1992).
virtual.yosemite.cc.ca.us /ghayes/granite.htm   (1080 words)

  
 Great Stone Dome and the Global Flood
An infinitely long batholith that is 11 km wide, 16.5 km thick, and is buried 20 km below the surface of the ground, when at zero rock permeability (that is, conductive cooling only) needs a few million years to cool.
This was then intruded by the batholith which metamorphosed the sediments next to the stock.
David Tyler will say that the batholith cooled off quickly, but it was originally under a mile of sediment and even if we grant that hydrothermal flow cools the batholith, according to the Creationist, Woodmorappe, such things would require about 3000 years.
home.entouch.net /dmd/greatstonedome.htm   (742 words)

  
 batholith nevada sierra   (Site not responding. Last check: 2007-11-06)
The current Sierra batholith was forming below the earth's surface in huge plumes of magma that were...
The lake is fed by Reverse Creek, which runs west toward the Sierra batholith instead of away from it.
One of the fundamental uncertainties about the Sierra Nevada batholith is the extent of the root to this mountain range:...
www.nevada-bookmarks.com /batholith_nevada_sierra.html   (392 words)

  
 Only in Butte -- Basking in the Boulder Batholith
Complex geology is to blame; it has made Butte what it was and what it is. Butte is in the heart of a huge granite formation called the Boulder Batholith that stretches from south of Helena to north of Dillon.
The Batholith was shaped by magma shoved upwards by volcanic eruptions about 60 to 70 million years ago.
To the East of Butte over Homestake Pass on I-90 the Batholith results in a crazy assortment of ruddy boulders on the east side of the pass that is known locally as The Dragonback.
www.butteamerica.com /batholith.htm   (550 words)

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