Mafic rocks pdf file

The term is a portmanteau, made up from magnesium and ferric mafic minerals are usually dark in color and have a specific gravity greater than 3. Pdf mafic and ultramafic rocks, and platinum mineralisation. Compositional trend of amphiboles in the mafic rocks from the. Due to the color of the minerals forming them, the rocks are either light or dark. Any calculation obviously depends on the directory path too, so deciding to archive andor adding a date or something else to make it unique could be enough to push new files.

Felsic, intermediate and mafic igneous rocks differ in their mineral composition. Mafic minerals are generally dark in colour usually green, brown or black. They occur in a high proportion of terrestrial mafic and ultramafic rocks, and a very large volume of microprobe data is available on their compositions. This page was last edited on 25 december 2019, at 03. The sapat maficultramafic complex, kohistan arc, north pakistan article pdf available in geological society london special publications 741. A mixture of minerals implies the presence of more than one mineral grain, but not necessarily more than one type of mineral. Pdf the sapat maficultramafic complex, kohistan arc. Examine one thin section from each of the following groups and provide a sketch, rock description and rock name.

Common rockforming mafic minerals include olivine, pyroxene, amphibole, biotite and other micas, augite and the calcium. In terms of chemistry, felsic rocks are on the other side of the rock spectrum from the mafic rocks. Multiple generations of maficultramafic rocks from the. Now we will examine some mafic and intermediate plutonic rocks under the microscope. Ultramafic rocks comprised of forty to one hundred percent percent olivine. In practice, this means that the average dimension of the crystals is less than 1 millimeter. Rocks formed from lava are extrusive, or volcanic rocks. An igneous rock or a part of an igneous rock with a finegrained or aphanitic texture has crystals, but they are too small to recognized with the unaided eye. What acreage or percentage of the continental us is covered by ultramafic mafic rocks. Mafic lava, before cooling, has a lower viscosity than felsic lava due to its lower silica content. Range of spinel compositions in terrestrial mafic and.

I guess that in x6 they have made a start, but it isnt fixed quite yet. Common mafic rocks include basalt, diabase and gabbro. Mostly k spar no quartz syenite pegmatitic mostly feldspar. How are felsic, intermediate and mafic igneous rocks. Most of these rocks are gray though mafic rocks are also found in brown, green, and even black colors. These minerals are high in magnesium and ferric oxides, and their presence gives mafic rock its characteristic dark colour. Compositional trend of garnet and feldspar in the mafic rocks from the hongseong area of the gyeonggi massif, south korea. Contain variable but greater than 10% of both ortho and clinopyroxene, and accessory phases. What acreage or percentage of the continental us is covered by ultramaficmafic rocks. Reserves were estimated in 1950 to be 840 t assaying 42. Igneous hypabyssal mafic hypabyssal hypabyssalbasalticandesite stock or pipe comments gabbro dikes, sills, and at least one plug intrude steens basalt in northern pueblo mountains and are substantial in size, but too small to appear on state geologic map or252. Ophiolites and other maficultramafic complexes in alaska by w.

Pdf intrusive rocks in the longwood range represent a component of the permian brook street terrane. They are usually light in colour and have specific gravities less than 3. How to classify igneous rocks into ultramafic, mafic. C1 rocks and magmas a rock is defined as a consolidated mixture of minerals. A rock can be composed of only one type of mineral. Mafic rocks are darker and are composed of magnesium and iron. Mafic rock, in geology, igneous rock that is dominated by the silicates pyroxene, amphibole, olivine, and mica. The most common examples of rocks classified as mafic are gabbro, dolerite, and basalt. Igneous rocks form from cooling and crystallization of molten rock magma. Magma molten rock within the earth lava molten rock on the earths surface. F if water unavailable, mafic igneous rocks will remain largely unaffected, even as associated sediments are completely re equilibrated.

Mafic volcanic rocks are melanocratic to mesocratic igneous rock which crystallized from a basaltic magma within the oceanic and continental. The complex is similar in composition to part of the mafic and ultramafic rock complex at iron. I am doing a graduate thesis on soils formed from ultramafic mafic rocks in the ga piedmont at the university of georgia, and i cannot seem to find an answer to this deceptively simple question. Identify igneous rockforming minerals based on their optical properties demonstrate the operation of the petrographic microscope in plane and crossed polarized light. Igneous rocks form as molten rock cools and solidifies general characteristics of magma. The derivation of the term is ma for magnesium and fic for iron from ferric. Part or all of this report is presented in portable document format pdf. Maficultramafic igneous rocks and associated carbonatites of the. Rocks that do not contain a lot of silica silicapoor tend to be dark in color and dense. Volumetrically small ultramafic layers occur plagioclase wehrlite, and thin veins of felsic rocks ranging from quartz diorite to trondhjemite. Mafic is an adjective describing a silicate mineral or igneous rock which is rich in magnesium and iron.

Mafic and ultramafic xenoliths from volcanic rocks of the western united states. Since new minerals are created during metamorphism, the end product metamorphic. A dyke is an intrusive body that is discordant with the country rock. Of the oxides, silica sio 2 is usually the most abundant. Felsic and mafic rocks, division of igneous rocks on the basis of their silica content.

Perley introducfion mafic and ultramafic rocks which have been metamor phosed to various degrees, are relatively common throughout the appalachian blue ridge and piedmont provinces figure 1. Mafic rock is commonly contrasted with felsic rock, in which. Most mafic minerals are dark in color, and common rockforming mafic minerals include olivine, pyroxene, amphibole, and biotite. Geochronology, geochemistry, and petrogenesis of late. Ultramafic rocks are dominated by pyroxene or olivine, and may contain a small amount of calciumrich plagioclase. Chemical analyses of the most abundant components in rocks usually are presented as oxides of the elements. Mineralogic contents felsic rock, with predominance of quartz, alkali feldspar andor feldspathoids. Mafic is a term used by geologists to describe igneous rocks and minerals. For best results viewing and printing pdf documents, it is recommended that you download the documents to your. Files are available under licenses specified on their description page. Mafic and ultramafic xenoliths from volcanic rocks of the. Medlin and hurst 1967 examined the greene county area and mapped amphibo lite with quartz megacrysts metagabbro.

In order for a rock to be classified as felsic, it generally needs to contain more than 75% felsic minerals. The term roughly corresponds to the older basic rock class. Please note that some geologists with questionable motives switch the order of the magnesium and iron and come up with the term femag. Plagioclase makes up the continuous reaction series. Mafic rocks have between 45 and 55% of silica, whereas felsic rocks have over 65% of silica, the highest of all types. Isotopic evidence suggests that the primary source of the.

Felsic simple english wikipedia, the free encyclopedia. The minerals found in these types of deposits and the deposit types themselves are described and discussed individually, mineral resource tracts and areas of interest are. Represents fertile mantle that has not undergone a melt extraction event. Intermediate rocks are composed of the minerals amphibole and feldspar and contain a combination of light and dark minerals. Publications on spinels particularly chromites have routinely used compositional fields based on the spinel prism to compare populations of analyses.

Mafic simple english wikipedia, the free encyclopedia. The mesoproterozioc 1600 to ma is repre sented by the namaqua metamorphic complex in the south, which comprises granitic gneisses, metasediments and felsic to mafic instrusions, and by the volcano sedimentary sinclair supergroup of central namibia, with its associated granites e. Mountain, about 9 miles to the northeast in the mcclure. I am doing a graduate thesis on soils formed from ultramaficmafic rocks in the ga piedmont at the university of georgia, and i cannot seem to find an answer to this deceptively simple question. The most common felsic rock is granite, but others include quartz, muscovite, orthoclase, and the. Felsic rocks are light in color and are composed of feldspars and silicates. Mafic rocks, including the volcanic rocks and dolerites from this study, crop out in the cenxi and wuzhou areas at the ne end of the dsgc belt fig. Geological survey editorial standards or with the north american stratigraphic code. Highly heterogeneous late mesozoic lithospheric mantle beneath the north china craton. Hopkins 1914 was the first to describe mafic rocks in eastcentral georgia as a belt of hornblende gneiss and gabbrodiorite which extends from monroe county northeastward to elbert county.

Mafic rocks that constitute the igneous oceanic crust are created at midocean ridge seafloor spreading centers as a byproduct of partial melt from upwelling. Mafic rocks are rich in minerals such as pyroxenes and amphiboles. Mafic is an adjective describing a silicate mineral or igneous rock that is rich in magnesium and iron, and is thus a portmanteau of magnesium and ferric. F hydration of original mafic minerals generally required. Felsic is a term that is used to refer to igneous rocks rich in mineral feldspar. Ultramafic rocks also referred to as ultrabasic rocks, although the terms are not wholly equivalent are igneous and metaigneous 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. Metamorphism of mafic rocks l clinopyroxene breaks down to a number of mafic minerals, depending on grade. Therefore, rocks are divided into ultramafic, mafic, intermediate, and felsic. Geology 111 b4 rocks and magmas vancouver island university.

Mafic and ultramafic rocks, and platinum mineralisation potential, in. Difference between mafic and felsic compare the difference. Mafic and intermediate plutonic rocks learning goals. Pdf the main mafic dyke swarms of the sao francisco craton range in age from late archean to the early neoproterozoic, and record extensional and. All structured data from the file and property namespaces is available under the creative commons cc0 license. Choose the best possible answer to the following questions about key concept 3 compositions of igneous rocks and their meaning. Includes the monument dike swarm of northwestern grant county or061, the chief. This lesson will examine the definition of this term and how to relates to earth processes. Silica content in mafic rocks is around 50% by weight. Igneous rocks and processes revised on 102011 page 5 of 10 finegrained or aphanitic. Chemically speaking, theyre rich in magnesium and iron. Mineral deposits related to mafic igneous rocks include podiform chromite, ultramafichosted talcmagnesite, and serpentinehosted asbestos. Rocks that contain a significant amount of silica silicarich tend to be light in color and not as dense. Tracing the styles of maficfelsic magma interaction.

Igneous rocks form the framework for the earths crust. Mafic magmas are usually produced at spreading centers, and represent material which is newly differentiated from the upper mantle. Relating to or containing a group of darkcolored silicate minerals, composed chiefly of magnesium and iron, that occur in igneous rocks, including. In other words, if the rock it intrudes into is in horizontal layers, a dyke would cut the layers. In terms of chemistry, mafic rocks are on the other side of the rock spectrum from the socalled felsic rocks. They provide an opportunity to explore the interaction between crust and mantle and to refine the tectonic setting of uht metamorphism and hightemperature magmatism in the dsgc belt. Greenishgray to dusky green, fine to mediumgrained, massive to amygdaloidal metabasalt with darkgray to white, mediumgrained mafic lithic and crystal tuff, and minor purple phyllite and metasedimentary rocks. The three minerals at the bottom do not form by reaction with the firstformed crystals. At kohikalawur, along the southeast foot of kohe saymahmude ghazi east of the logar river, seven chromite lenses as much as 4. Endnote needs a tool to run to shorten all the pdf and pdf folder names for existing libraries.

Dikes, plugs, and sills of basalt, diabase, gabbro, and lesser andesite that fed many of the miocene basalt and andesite flows in units tc and tba. Metamorphic rocks metamorphic rocks are rocks from sedimentary and igneous origin that have been changed through high pressures and temperatures during orogenesis mountain building or during igneous intrusion contact metamorphism metamorphic rocks cont. Pdf the sapat maficultramafic complex, kohistan arc, north. Basement here refers to the crystalline layer of variable composition below the oldest dated sequence of sedimentary, volcanic, or metamorphic rocks. Parent material of igneous rocks forms from partial melting of rocks magma at surface is called lava general characteristics of magma general characteristics of magma.