Similarities between Basalt and Ophiolite
Basalt and Ophiolite have 33 things in common (in Unionpedia): Archean, Back-arc basin, Bowen's reaction series, Breccia, Calc-alkaline magma series, Chlorite group, Diabase, Earth's mantle, Epidote, Extrusive rock, Feldspar, Gabbro, Hotspot (geology), Hydrothermal circulation, Hydrothermal vent, Igneous rock, Intrusive rock, Iron, Magma, Mid-ocean ridge, Oceanic crust, Olivine, Ore, Peridotite, Plagioclase, Plate tectonics, Pyroxene, Quartz, Silicon dioxide, Subduction, ..., Titanium dioxide, Ultramafic rock, Upper mantle. Expand index (3 more) »
Archean
The Archean Eon (also spelled Archaean or Archæan), in older sources sometimes called the Archaeozoic, is the second of the four geologic eons of Earth's history, preceded by the Hadean Eon and followed by the Proterozoic.
Archean and Basalt · Archean and Ophiolite ·
Back-arc basin
A back-arc basin is a type of geologic basin, found at some convergent plate boundaries.
Back-arc basin and Basalt · Back-arc basin and Ophiolite ·
Bowen's reaction series
Within the field of geology, Bowen's reaction series is the work of the Canadian petrologist Norman L. Bowen, who summarized, based on experiments and observations of natural rocks, the sequence of crystallization of common silicate minerals from typical basaltic magma undergoing fractional crystallization (i.e. crystallization wherein early-formed crystals are removed from the magma by crystal settling, leaving behind a liquid of slightly different composition).
Basalt and Bowen's reaction series · Bowen's reaction series and Ophiolite ·
Breccia
Breccia is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix.
Basalt and Breccia · Breccia and Ophiolite ·
Calc-alkaline magma series
The calc-alkaline magma series is one of two main subdivisions of the subalkaline magma series, the other subalkaline magma series being the tholeiitic series.
Basalt and Calc-alkaline magma series · Calc-alkaline magma series and Ophiolite ·
Chlorite group
The chlorites are the group of phyllosilicate minerals common in low-grade metamorphic rocks and in altered igneous rocks.
Basalt and Chlorite group · Chlorite group and Ophiolite ·
Diabase
Diabase, also called dolerite or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro.
Basalt and Diabase · Diabase and Ophiolite ·
Earth's mantle
Earth's mantle is a layer of silicate rock between the crust and the outer core.
Basalt and Earth's mantle · Earth's mantle and Ophiolite ·
Epidote
Epidote is a calcium aluminium iron sorosilicate mineral.
Basalt and Epidote · Epidote and Ophiolite ·
Extrusive rock
Extrusive rock refers to the mode of igneous volcanic rock formation in which hot magma from inside the Earth flows out (extrudes) onto the surface as lava or explodes violently into the atmosphere to fall back as pyroclastics or tuff.
Basalt and Extrusive rock · Extrusive rock and Ophiolite ·
Feldspar
Feldspar (sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium.
Basalt and Feldspar · Feldspar and Ophiolite ·
Gabbro
Gabbro is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface.
Basalt and Gabbro · Gabbro and Ophiolite ·
Hotspot (geology)
In geology, hotspots (or hot spots) are volcanic locales thought to be fed by underlying mantle that is anomalously hot compared with the surrounding mantle.
Basalt and Hotspot (geology) · Hotspot (geology) and Ophiolite ·
Hydrothermal circulation
Hydrothermal circulation in its most general sense is the circulation of hot water (Ancient Greek ὕδωρ, water,Liddell, H.G. & Scott, R. (1940). A Greek-English Lexicon. revised and augmented throughout by Sir Henry Stuart Jones. with the assistance of. Roderick McKenzie. Oxford: Clarendon Press. and θέρμη, heat). Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earth's crust.
Basalt and Hydrothermal circulation · Hydrothermal circulation and Ophiolite ·
Hydrothermal vent
Hydrothermal vents are fissures on the seabed from which geothermally heated water discharges.
Basalt and Hydrothermal vent · Hydrothermal vent and Ophiolite ·
Igneous rock
Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic.
Basalt and Igneous rock · Igneous rock and Ophiolite ·
Intrusive rock
Intrusive rock is formed when magma penetrates existing rock, crystallizes, and solidifies underground to form intrusions, such as batholiths, dikes, sills, laccoliths, and volcanic necks.
Basalt and Intrusive rock · Intrusive rock and Ophiolite ·
Iron
Iron is a chemical element.
Basalt and Iron · Iron and Ophiolite ·
Magma
Magma is the molten or semi-molten natural material from which all igneous rocks are formed.
Basalt and Magma · Magma and Ophiolite ·
Mid-ocean ridge
A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics.
Basalt and Mid-ocean ridge · Mid-ocean ridge and Ophiolite ·
Oceanic crust
Oceanic crust is the uppermost layer of the oceanic portion of the tectonic plates.
Basalt and Oceanic crust · Oceanic crust and Ophiolite ·
Olivine
The mineral olivine is a magnesium iron silicate with the chemical formula.
Basalt and Olivine · Olivine and Ophiolite ·
Ore
Ore is natural rock or sediment that contains one or more valuable minerals concentrated above background levels, typically containing metals, that can be mined, treated and sold at a profit.
Basalt and Ore · Ophiolite and Ore ·
Peridotite
Peridotite is a dense, coarse-grained igneous rock consisting mostly of the silicate minerals olivine and pyroxene.
Basalt and Peridotite · Ophiolite and Peridotite ·
Plagioclase
Plagioclase is a series of tectosilicate (framework silicate) minerals within the feldspar group.
Basalt and Plagioclase · Ophiolite and Plagioclase ·
Plate tectonics
Plate tectonics is the scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
Basalt and Plate tectonics · Ophiolite and Plate tectonics ·
Pyroxene
The pyroxenes (commonly abbreviated Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks.
Basalt and Pyroxene · Ophiolite and Pyroxene ·
Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide).
Basalt and Quartz · Ophiolite and Quartz ·
Silicon dioxide
Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula, commonly found in nature as quartz.
Basalt and Silicon dioxide · Ophiolite and Silicon dioxide ·
Subduction
Subduction is a geological process in which the oceanic lithosphere and some continental lithosphere is recycled into the Earth's mantle at convergent boundaries.
Basalt and Subduction · Ophiolite and Subduction ·
Titanium dioxide
Titanium dioxide, also known as titanium(IV) oxide or titania, is the inorganic compound derived from titanium with the chemical formula.
Basalt and Titanium dioxide · Ophiolite and Titanium dioxide ·
Ultramafic rock
Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).
Basalt and Ultramafic rock · Ophiolite and Ultramafic rock ·
Upper mantle
The upper mantle of Earth is a very thick layer of rock inside the planet, which begins just beneath the crust (at about under the oceans and about under the continents) and ends at the top of the lower mantle at.
The list above answers the following questions
- What Basalt and Ophiolite have in common
- What are the similarities between Basalt and Ophiolite
Basalt and Ophiolite Comparison
Basalt has 260 relations, while Ophiolite has 126. As they have in common 33, the Jaccard index is 8.55% = 33 / (260 + 126).
References
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