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Category of coarse-grained igneous rocks
A granitoid is a broad term referring to a diverse group of coarse-grained igneous rocks that are widely distributed across the globe, covering a significant
Granitoid
Type of igneous rock
kilometers. Granite is typical of a larger family of granitic rocks, or granitoids, that are composed mostly of coarse-grained quartz and feldspars in varying
Granite
Felsic volcanic rocks formed in the Archean Eon
are important to reconstruct Archean geological environments. Felsic granitoids are the most prevalent rock type in Archean terranes. These intrusive
Archean_felsic_volcanic_rocks
Multicoloured metamorphic rock
Unakite is a coarse-grained metamorphic rock that is an altered granitoid composed of orthoclase feldspar (pink), epidote (yellow-green), and quartz (smokey
Unakite
Sand and gravel fragments accumulation
chemical and mechanical weathering of crystalline rocks (most notably granitoids), generally in an arid or semiarid region. Grus sand, when cemented into
Grus_(geology)
Part of the Indian Shield in south India
gneisses, volcanic-sedimentary greenstone sequences and calc-alkaline granitoids. The western Dharwar Craton contains the oldest basement rocks, with greenstone
Dharwar_Craton
United States historic place
R.S. Blome Granitoid Pavement is a historic road surface, as well as the associated cut sandstone curbs in a few sections, found in three of the oldest
R.S. Blome Granitoid Pavement in Grand Forks
R.S._Blome_Granitoid_Pavement_in_Grand_Forks
Intrusive igneous rock
occurs in relatively small concentrations (< 5%). It is considered a granitoid. Some syenites contain larger proportions of mafic components and smaller
Syenite
Type of sedimentary rock
Grus sand and the granitoid from which it is derived
Sandstone
Archaean craton, possibly part of the Vaalbara supercontinent
formed and stabilised between 3.7 and 2.6 Ga by the emplacement of major granitoid batholiths that thickened and stabilised the continental crust during
Kaapvaal_Craton
Greenstone belt that spans across the Ontario–Quebec border in Canada
volcanic rocks, but also includes ultramafic rocks, mafic intrusions, granitoid rocks, and early and middle Precambrian sediments. The Abitibi greenstone
Abitibi_greenstone_belt
Prehistoric impact crater in Mexico
interpreted to have formed in the Pan-African orogeny. Late Paleozoic granitoids (the distinctive "pink granite") were found in the peak ring borehole
Chicxulub_crater
Mountain in Nova Scotia, Canada
range is also known as the South Mountain Batholith, the largest body of granitoid rocks in the entire Appalachians and comprises both granite barrens and
South_Mountain_(Nova_Scotia)
Mountain in Italy
The ridge is composed of two different rock formations, one made up of granitoid gneiss, the other of mixed gneiss and different kinds of migmatite. The
Monte_Matto
Mountain in Italy
Geologically, the mountain is formed by granitoid gneiss, with outcrops of amphibolic agmatites (granitoid migmatites). It may be climbed from the Refuge
Monte_Clapier
Mountain in Italy
it is part of the Mercantour-Argentera massif, and is mostly formed by granitoid gneiss. The peak is composed of two smaller ones, divided by a gorge;
Cime_du_Gélas
Foliation in granitoids
Magmatic foliation is a term in geology, for foliation in granitoids that form by magmatic flow, "submagmatic flow," by high-temperature solid-state deformation
Magmatic_foliation
island of Bornholm in the Baltic Sea. Common rocks in the province are granitoids, orthogneiss and migmatite formed in the Late Paleoproterozoic next to
Blekinge-Bornholm_Province
Mountain range in Russia
Triassic, Jurassic and Cretaceous Rock types Shale, mudstone, siltstone, Sandstone, granite and granitoid intrusions Climbing Easiest route From Batagay
Kisilyakh_Range
Group of rock units in the Yangtze Block, South China
Kongling Complex. The middle of the core is mainly the Neoproterozoic granitoid. The southern part of the core is the Neoproterozoic potassium granite
Huangling_Anticline
Mineral-rich region in Southeast Asia
approximately 400 km wide. It is geologically associated with a series of granitoid intrusions following the same trend as the tin belt. The particular intrusions
Southeast_Asian_tin_belt
Type of rock found in Finland
Vaasa granite is a migmatitic Paleoproterozoic garnet-bearing granitoid with variable amounts of gneissose enclaves. The name refers to occurrences at
Vaasa_granite
Subtype of granite formed in anorogenic or anhydrous conditions
particular category of the S-I-A-M or 'alphabet' system which classifies granitoids and granitic rock by their protoliths or source. The 'A' stands for Anorogenic
A-type_granite
economically significant Peridotite Nappe. This is followed by intrusions of granitoids into the country rocks on Grande Terre. Since then, the Island re-emerged
Geology_of_New_Caledonia
City in North Dakota, United States
unique architectural styles. This neighborhood has areas of original granitoid paving, several historic churches, and Lincoln Drive Park. The Near Southside
Grand_Forks,_North_Dakota
Ancient oceanic tectonic plate
subduction generated a continental-margin volcanic arc, producing widespread granitoid intrusions within the continental interior. By the Early to Middle Jurassic
Intermontane_terranes
District in the state of Chhattisgarh, India
(1998–2015) Yellow soils (Ultisols) and red soils (Alfisols) developed over the granitoids occupy most part of the district Black soils (Inceptisols) have formed
Jashpur_district
igneous rock – A plutonic rock dominated by orthoclase feldspar; a type of granitoid Syenogranite – Intrusive igneous rock of the granite family Tachylyte –
List_of_rock_types
Township in Tibet Autonomous Region, China
canola, is predominant.[citation needed] Geologically, Late Triassic granitoids in the area are mainly "exposed in a fault uplift in the Gangdise tectonic
Mamba_Township
Mediterranean island in Tuscany, Italy
and the intrusion of the Mount Capanne and the La Serra-Porto Azzuro granitoids. These igneous bodies brought with them skarn fluids which dissolved and
Elba
granitoid Chaillu Massif spanning into the Republic of Congo through Gabon. The massif has a north–south foliation and two generations of granitoids.
Geology of the Democratic Republic of the Congo
Geology_of_the_Democratic_Republic_of_the_Congo
Standing stone on the Hill of Tara, Ireland
quarry sites.[citation needed] It has also been identified as a whitish granitoid.[needs independent confirmation] There are several different, and conflicting
Lia_Fáil
Japan north of Japan Median Tectonic Line ("Inner Zone") contains many granitoid fragments dating from Paleogene to Cretaceous period intruding the older
Geology_of_Japan
Ancient granite-greenstone terrane in South Africa
metasedimentary rocks emplaced and deposited between 3.5 and 3.2 Ga. The granitoid rocks were emplaced over a 500-million-year time span and can be divided
Barberton_Greenstone_Belt
Mountain in the U.S. state of Utah
the summit. Lone Peak consists almost entirely of quartz monzonite (a granitoid or granite-like rock) of the 30.5 million-year-old Little Cottonwood Stock
Lone_Peak_(Utah)
Mountain range in the Eastern U.S.
geology of the Blue Ridge is made of compositionally unique gneisses and granitoids, including orthopyroxene-bearing charnockites. Analysis of zircon minerals
Blue_Ridge_Mountains
Geological formation in Ontario, Canada
The Spawning Lake Stock is an Archean age granitoid stock in Northeastern Ontario, Canada, located in Briggs Township and Chambers Township of Temagami
Spawning_Lake_Stock
Ancient supercontinent of approximately 2,500 to 1,500 million years ago
7–1.6 Ga Kongsberggian-Gothian Belt, and 1.5–1.3 Ga Southwest Sweden Granitoid Belt in Baltica. Other cratonic blocks also underwent marginal outgrowth
Columbia_(supercontinent)
Mountain range in Millard County, Utah, USA
Cambrian to Devonian carbonate rock which was intruded by a pink Jurassic granitoid in the central part of the range. In the Wheeler Amphitheater, away from
House_Range
Increasing mineral diversity over time
mineral evolution. Given sufficient heat, basalt was remelted to form granitoids, coarse-grained rocks similar to granite. Cycles of melting concentrated
Mineral_evolution
HREE are primarily enriched in granitoids through two separate mechanisms. LREE enrichment: LREE-enriched granitoids are formed by magma differentiation
Regolith-hosted rare earth element deposits
Regolith-hosted_rare_earth_element_deposits
Ancient Egyptian princess and priestess, God's Wife of Amun
small objects including scarabs. A statue of Amenirdis I carved from granitoid and decorated in gold leaf is held by the Nubian Museum in Aswan, Upper
Amenirdis_I
Type of igneous rock
Scottish appinites – get tied up with active subduction, the formation of granitoids and also the termination of subduction by slab breakoff. In the case of
Appinite
Neighborhood in Knoxville, Tennessee, United States
is characterized by short front lawns and large sidewalks. Circa-1907 "Granitoid" pavement, known locally as "singing" pavement due to the sound it makes
Old_North_Knoxville
Park in Ohio, United States
southwest corner's rock contains a plaque reading "Glacial boulder of granitoid gneiss from eastern Canada, excavated from 10 feet below the surface of
Tappan_Square
Geologic formation in Temagami, Ontario, Canada
Temagami, Northeastern Ontario, Canada. It is one of the three separate granitoid intrusions that constitute the Temagami Greenstone Belt, consisting of
Iceland_Lake_Pluton
Geologic complex in Northeastern Ontario, Canada
Chambers-Strathy Batholith, also called the Strathy-Chambers Batholith, is a large granitoid batholith complex in the Temagami region of Northeastern Ontario, Canada
Chambers-Strathy_Batholith
Hazardous group of rocks southwest of Britain
which is part of a considerable underwater outcrop of mica-schists and granitoid gneisses which are not found elsewhere in South West England. Research
Eddystone_Rocks
can even be dated back to the Precambrian times. The multiple stages of granitoid emplacements through its geological history have made Hainan Island rich
Geology_of_Hainan_Island
Sally; Morris, Clyde; McCrosky, Lauren (August 23, 1991). "R.S. Blome Granitoid Pavement in Grand Forks". National Register of Historic Places Registration
National Register of Historic Places listings in Grand Forks County, North Dakota
National_Register_of_Historic_Places_listings_in_Grand_Forks_County,_North_Dakota
of Archean crust led to widespread basin formation. A large magmatic, granitoid forming event during the orogeny produced rocks with unusually similar
Barramundi_orogeny
Inferred fault bounded terrane of the basement rocks of the southern United Kingdom
However, there are outcrops of the Parwyd Gneiss which are retrogressed granitoid gneiss and garnet amphibolite that occur with the Llyn Shear Zone. This
Cymru_terrane
orogeny is associated with intense igneous activity that produced large granitoid plutons. The event lined up with the Katarchean, a period in which the
Saamian_orogeny
basaltic rocks (eg. lava, hyaloclastites) along with smaller quantities of granitoids, metasedimentary rocks and gneiss. Recovered samples from the North Scotia
West_Scotia_Basin
Multi-day trekking route in southern Vietnam
Bình Thuận associated with intrusive and metamorphic bedrock, including granitoid complexes. The transition produces contrasts between rolling hill surfaces
Ta_Nang-Phan_Dung_trail
Buyantuev, M.D.; Antsiferova, T.N.; Karavaeva, G.S. (2016). "Late Paleozoic granitoid magmatism of Eastern Kazakhstan and Western Transbaikalia: plume model
Angara-Vitim_batholith
Biotite granite rocks that are considered to be the final fractionation product of magma
Vigo–Régua shear zone, the monzogranites belong to the syn-F3 biotite granitoid group. They include large crystals of potassium feldspar and have enclaves
Monzogranite
Ocean in South America in Neoproterozoic
Craton. Its closure started with a magmatic arc forming (now seen as granitoids of the Guaxupé and Socorro Nappes) and eventually gave rise to the Brasiliano
Goianides_Ocean
Set of lakes in Washington, United States
272 ft) Sorcery Mountain, and 1,610 metres (5,280 ft) Galleon Mountain. Granitoid ridges near the lake rise to about 3,425 feet (1,044 m) above sea level
Snoqualmie_Lake_Potholes
Unclaimed West Antarctic region
rock in MBL is Paleozoic metamorphosed sedimentary rock and granitoid, and Mesozoic granitoid. Away from the coasts, the WAIS buries individual mountains
Marie_Byrd_Land
mostly of marine-sedimentary and submarine-volcanic origin, intruded by granitoid plutons. Most of these rocks are of late Carboniferous age or older. Folding
Geology_of_Germany
the Zimbabwe Craton, a core of Archean basement composed in the main of granitoids, schist and gneisses. It also incorporates greenstone belts comprising
Geology_of_Zimbabwe
Municipality in Nitra Region, Slovakia
to the Nitra Region and Nitra District. Its territory is built up of granitoid and sedimentary rocks (granites, quartzites, limestones, clays, sands)
Jelenec
diamictites. Post-Minas intrusives (various ages): Pegmatitic dikes and granitoid plutons which intruded into the Minas Supergroup. It is these pegmatites
Iron_Quadrangle
Zirconium silicate mineral
(1994). "Systematics of internal zircon morphology in major Variscan granitoid types". Contributions to Mineralogy and Petrology. 117 (4): 331–344. Bibcode:1994CoMP
Zircon
Study of the mechanical behavior of rocks
Grus sand, and the granitoid from which it is derived
Rock_mechanics
Lake and claimed impact structure in Karelia, northwest Russia
megabreccias. The megabreccias are composed of blocks of both basement granitoids and supracrustal greenstone. Shock metamorphic features in are reported
Suavjärvi
Unincorporated community in Newfoundland and Labrador, Canada
Central Mineral Belt, Labrador: General geology and description of regional granitoid units" (PDF). Newfoundland Department of Mines and Energy: 89–100.
Adlavik_Islands
Archean age, are found in the east and north. These rocks are chiefly granitoids and migmatitic gneiss. Rocks in central and western Finland originated
Geology_of_Finland
Place in Northern Cape, South Africa
orbicular diorite in the country, the rare rock texture is the result of granitoid magmas separating while in a fluid state which forms concentric internal
Concordia,_South_Africa
within the metamorphic rock. Strontium-argon dating of the Motajica granitoid returned an age of 48 million years ago. After the formation of the Dinaride
Geology of Bosnia and Herzegovina
Geology_of_Bosnia_and_Herzegovina
Outcrop in Death Valley National Park, USA
composites having less than 20% quartz composition are referred to as granitoids. It was exposed on the surface during the Pleistocene epoch, as were Ubehebe
The_Grandstand
Late Oligocene to Early Miocene sedimentary formation in the Sierra Pelona of California
Jurassic granitoid were encountered in the Vasquez Formation. North of Blue Ridge, the Vasquez Formation also lies depositionally atop granitoid, possibly
Vasquez_Formation
Craton: A Simple Story for an Intricate Igneous Complex Early precambrian A-granitoids in the Aldan Shield and adjacent mobile belts: Sources and geodynamic
Aldan_Shield
Wilderness area in Utah and Salt Lake counties in Utah, United States
The geologic structure of the area is varied and complex, consisting of granitoid rock masses and several sedimentary formations. The carving of the present
Lone_Peak_Wilderness
Igneous rock
cotectic systems: A review of experimental studies with applications to granitoid petrogenesis". Earth-Science Reviews. 124: 68–95. doi:10.1016/j.earscirev
Tonalite
covering most of Hälsingland. The Ljusdal Bathoilith is mostly made up of granitoids with lesser amounts of mafic intrusions. The plutons of the batholith
Ljusdal_Batholith
generations of plutons: Silurian to Early Devonian (440-400 million years old) granitoids and middle Carboniferous (Hercynian, 340-325 million years old) granites
Mid-German_Crystalline_High
different belts are basins filled with dacite, argillite, volcaniclastic and granitoid rocks with isocline folding. At the transition between the basins and
Geology_of_Ghana
Mountain summit of the Sierra Nevada mountain range in California
Langley Geology Rock age Cretaceous Mountain type Fault block Rock type Granitoid Climbing First ascent 1933 by Howard S. Gates Easiest route Scramble (class 2–3)
Mount_Corcoran
Geologic eon, 2500–539 million years ago
happened episodically. By isotopically calculating the ages of Proterozoic granitoids it was determined that there were several episodes of rapid increase in
Proterozoic
Mountain in the Czech Republic
chlorite, and muscovite), gneisses, quartzites, igneous rocks (mainly meta-granitoids), and sedimentary rocks, primarily meta-conglomerates and meta-siltstones
Lyra_(mountain)
Naturally occurring mineral aggregate
igneous rock of mafic composition. Granite and similar rocks, known as granitoids, dominate the continental crust. Sedimentary rocks are formed at the earth's
Rock_(geology)
Department of France
undulating plateau including three well-marked ranges of hills in the south. A granitoid chain, the Monts du Méné, starting in the south-east of the department
Côtes-d'Armor
Town in New South Wales, Australia
Cowra. The topography of the land is rough and hilly, featuring large granitoid tors and associated boulders. The area has a significant mining history
Darbys_Falls,_New_South_Wales
Tiny intergrowths of quartz and feldspar in rocks
This is the third type of quartz-feldspar intergrowth in metasomatic granitoids. Again this process depends on tectonically deformed crystals. In this
Myrmekite
Snow-free valleys in Antarctica
marble and calc schist. The Palaeozoic Granite Harbour intrusives include granitoid plutons and dykes, which intruded into the metasedimentary Skelton Group
McMurdo_Dry_Valleys
Type of sandstone containing at least 25% feldspar
sand in the Llano Uplift, Texas, with granite outcrops Grus sand and the granitoid it's derived from The central Australian inselberg Uluru (Ayers Rock)
Arkose
Craton mainly consists of two rock units: granitoid plutons (2.8–2.55 Ga) and gneiss and migmatite. The granitoid rocks are mainly potassic granite and were
Geology of the Rocky Mountains
Geology_of_the_Rocky_Mountains
Orogenic belt in southwestern Sweden and southern Norway
part of the terrane hosts the Sirdal Magmatic Belt which is made up of granitoids including orthogneiss. The igneous rocks of the Sirdal Magmatic Belt are
Sveconorwegian_orogeny
Stuckless, John S., 1989, Petrogenesis of two contrasting Late Archean granitoids, Wind River Range, Wyoming: USGS Professional Paper 1491, 38 p. 42°31′N
South_Pass_greenstone_belt
Part of the North Atlantic Craton in Labrador, Canada
varies between 28 and 38 km (17 and 24 mi) thick and its rocks are 85% granitoid gneisses. The Nain Province was intruded by the 1350- to 1290-million-year-old
Nain_Province
Paleozoic mountain building event in Antarctica
Antarctica. This is inferred from a large number of I-type and S-type granitoids which are similar to large circum-Pacific batholiths. During the Late
Ross_orogeny
Orogen that formed during the Neoproterozoic
rocks, granitoids and few ophiolites. In contrast the southwestern part of the orogen is made up mostly of sedimentary rocks. I and A type granitoids and
Timanide_Orogen
American geologist (1925–2022)
Taylor. "87Sr/86Sr and 18O/16O Isotopic Systematics and Geochemistry of Granitoid Plutons Across a Steeply Dipping Boundary Between Contrasting Lithologic
Leon_Silver
Oldest-surviving crustal material from the Hadean eon
apatite, ilmenite) and "S-type" (quartz, K-feldspar, muscovite, monazite) granitoids. Dominated by quartz with less abundant K-feldspar, plagioclase, muscovite
Hadean_zircon
One of the five Precambrian cratons that make up the African Plate
Paleoproterozoic domains made of greenstone belts, sedimentary basins, regional granitoid-tonalite-trondhjemite-granodiorite (TTG) plutons, and large shear zones
West_African_Craton
ISSN 0028-8306. Allibone, A. H.; Tulloch, A. J. (1997). "Metasedimentary, granitoid, and gabbroic rocks from central Stewart Island, New Zealand". New Zealand
Stratigraphy_of_New_Zealand
Metamorphic rock formed under high pressure
eclogite. (Merschat, et al., 2012) Transitional granulite-eclogite facies granitoid, felsic volcanics, mafic rocks and granulites occur in the Musgrave Block
Eclogite
Magnetic anomaly in Russia due to extensive presence of iron ore
quartzites disseminated throughout metamorphic rocks and Pre-Cambrian granitoids. Surveyed ore reserves of ferrous quartzite are presently estimated at
Kursk_Magnetic_Anomaly
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