Nov 18, 2019 foliation and lineation are two separate entities, but are often found complementing one another in the same metamorphic rocks, as you will see later. Both foliation and lineations features of deformation in rocks. Foliation, cleavage, lineation the terms foliation and cleavage in metamorphic rocks have formal definitions, but their colloquial use in the field is commonly haphazard and interchangeable. Lineation return to linear structures can be sedimentary e. Foliation is any penetrative planar fabric present in rocks. Foliated rocks typically appear as if the minerals are stacked like pages of a book, thus the use of the term folia, like a leaf. On account of the parallel disposition of the elongated clusters of dark and light mineral constituents in alternate bands, the nepheline syenites have been rendered gneissose.
What is the difference between foliation and lineation answers. The more planar surfaces there are in an exposure, the more potential intersections there will be. As nouns the difference between lineation and foliation is that lineation is geology a linear feature in rock, often structural while foliation is lb the process of forming into a leaf or leaves. Lineation, parallel to hammer, and conjugate joints in moine quartzite. Any mesoscopically penetrative subparallel alignment of planar fabric elements in a rock. Each layer may be as thin as a sheet of paper, or over a meter in thickness.
Working with foliation and signatures polonsky foundation. Learn vocabulary, terms, and more with flashcards, games, and other study tools. The pictures show how a schistosity fabric looks like on outcrop scale bottom left, on a large thin section top right, scale. Geometric relationships which result from reactivation of foliations around porphyroblasts can be used to aid determination of the timing of the growth. Foliation is exhibited most prominently by sheety minerals, such as mica or chlorite. Lineations related to plastic deformation ltectonite lineation forms the dominating fabric and the foliation s fabric is weak or absent. Aug 12, 2017 lineation may be defined in a more precise way as any linear fabric element. Lineation only, due to unidirectional stretching constriction ls. Ppt analysis of lineation and foliation rudra mohan. Schistosity foliation only due to flattening no lineation l.
To qualify as a foliation or lineation, a structure must be penetrative within a volume that has a dimension on the order of tens of centimeters. However, foliation is most welldevelopedthat is, the rock layers have experienced the greatest amount of flatteningin the gneisses and other coarsegrained rocks of high metamorphic grade which form under high pressure and in temperatures above 320 c 608 f. It is caused by shearing forces pressures pushing different sections of the rock in different directions, or differential. There is no or only weak lineation ltectonite alignment of linear fabric elements creates the dominant fabric, so the rock may split into rodlike shapes. Foliations and foliated vector bundles first installment, 14 john milnor the following is a revised version of lectures given at m. A fabric is built of minerals and mineral aggregates with a preferred orientation that penetrates the rock at the microscopic to centimeter scale. That the parallel lineation seen in the lower part is a result of transposition of a deformed lineation is indicated by the occurrence of apices of the folded form in some domains as in the upper part of the specimen.
Foliation refers to planeparallel alignment of planar or plateshaped features in a rock that developed during metamorphism. Foliation and lineation, related to noncoaxial strainshearing. A penetrative secondary foliation and lineation, defined by tectonically flattened and elongated fragments, are present in the onaping formation of the south. Foliation refers to planeparallel alignment of planar or plateshaped features in. Extreme ductile shearing in shear zones tends to reduce the grain size of mineral grains, while stretching the original grains out into domains of extreme dimensions, and also producing strong. Because of the low temperatures and pressure, we can label this type of. Lineations in structural geology are linear structural features within rocks. Nanotexture of penetrative foliation in metamorphic rocks. Foliation is a term used that describes minerals lined up in planes. Choose from 81 different sets of foliation flashcards on quizlet. The scribes and printers who produced these books didnt number the individual pages. These foliations are transversely orientable if, and only if, the manifold b is orientable. To interpret some common types of foliation and lineation in deformed rocks. Lineation is expressed by the parallelism of some directional property in the rock.
The authors have recognized strong lineation in the nepheline syenites of khammam district, andhra pradesh. An introduction to distributions and foliations samuel otten michigan state university mth 864 spring 2008 in smooth manifold theory, the notion of a tangent space makes it possible for di. Foliation and layering are the two terms related to the formation of rocks. The origin of foliation and lineation in the onaping formation and. Foliation and lineation 1 foliation and lineation goal to interpret some common types of foliation and lineation in deformed rocks 2 foliation mesoscopically penetrative subparallel alignment of planar fabric elements in a rock. Feb 20, 2009 lineation means that all the linear minerals or structures are lying parallel, like a stack of logs. Foliation in geology refers to repetitive layering in metamorphic rocks. Each layer can be as thin as a sheet of paper, or over a meter in thickness. Foliation fabric elements are planar and essentially parallel to one another, creating a 2dimensional fabric. Lineation means that all the linear minerals or structures are lying parallel, like a stack of logs. S foliation, and c foliation, both of which develop during the same deformation event. Foliation in feldsparrich metamorphic rock, formed at intermediate to high. Tectonites rocks that are pervaded by foliation, lineation and roll no.
Secondary foliations that are not homogeneous may be difficult to distinguish from primary layering box 4. Primary foliations are structures related to the origi nal rockforming process. A lineation is caused by a similar growth of elongate minerals eg. Letters indicate which planar features intersect b bedding f undifferentiated foliation p penetrative s spaced c crenulation a anastamosing mark equivalent fold asymmetry s,z or m where possible pervasive lineation such as mineral or shape fabric surface lineation such as slickenline. Rocks that are pervaded by foliation and or lineation flowed in solid state schistosity foliation only due to flattening no lineation. The lineation corresponds to the direction of maximum stretching x whitin the foliation plane xy.
By far the most common texture type has 010 poles nearly perpendicular to the foliation plane and 100 axes subparallel to the lineation direction fig. Geological background, rock mechanics significance. Lstectonite a strong foliation and a strong lineation. Typically, the flyleaves of a book are foliated with roman numerals, and arabic. For instance, according to the measurement conventions of structural geology, original bedding, s 0 intersected by a folds axial plane foliation, forms an intersection lineation l 01, with an azimuth and. Lineation defined by stretched pebbles in a conglomerate tectonites. Intersection lineations can also be due to the intersection of two foliations. Expand on fabric elements, mesoscopic, and penetrative typically forms in metamorphic rocks combines mineral shapepreferred orientation and compositional. Rocks exhibiting foliation include the standard sequence formed by the prograde metamorphism of mudrocks. Recent examples on the web but because according to general relativity spacetime is curved, there is no standard way to extend a local foliation to the entire universe. The term unfoliated gneiss is coined to describe such gneissic rocks with lineation alone and without planar arrangement foliation of the constituent mineral grains.
Combines mineral shapepreferred orientation and compositional banding. The word comes from the latin folium, meaning leaf, and refers to the sheetlike planar structure. Slate, schist, and gneiss are three common foliated metamorphic rocks. Foliation and lineation lecture 12 impact tectonics. Lstectonite balanced combination of foliation sfabric and a penetrative fabric lfabric. Its eventual goal is to describe the classifying space for codlmenslon g foliated manifolds which has recently been constructed by a. Foliation and layering involve different kinds of rock formation. Lineations however are indicatives of the presence of foliation but lineation is a planar stucture measured in therms of dip and. As shown in this example, one characteristic of slate foliation is the way in which these parallel lines appear in the rock. Fabric is used to describe the spatial and geometric relationships that make up the rock. Intersection lineations are measured in relation to the two structures which intersect to form them. In sedimentary and metamorphic rocks, foliation and layering is presented as a pattern.
Use ball indicating known top direction of layers only on maps where top direction may be in doubt elsewhere. Scribd is the worlds largest social reading and publishing site. It is caused by shearing forces pressures pushing different sections of the rock in different directions, or differential pressure higher. These include fractures, faults, folds, boudins, shear zones, cleavages also knows as schistosities, foliations and lineations. Lineation may be defined in a more precise way as any linear fabric element. What is the difference between lineation and foliation in. Nanotexture of penetrative foliation in metamorphic. North cascades, wa the rocks of the cascade core are characterized by pervasive lineation, generally much stronger than foliation. Foliation is the result of the parallel arrangement of micas, etc. This wilkerson diagram contains illustrations of rock behavior when a a foliation is present, b a lineation is present, and c when the rock contains a combination of the two, wilkerson.
This process is called folio numbering or foliation. What is the difference between foliation and lineation. The recognition of primary foliation is important, however, because in metasediments it allows recon. Table 1 determining view of the nanotexture of penetrative foliation in both regional metamorphic rocks and dynamic. Geological background, rock mechanics significance, and preliminary investigations at olkiluoto abstract a well developed, pervasive foliation is a characteristic feature of the migmatites and gneisses in the olkiluoto bedrock, and is expected to have a significant influence on the. Foliation definition is the process of forming into a leaf. The trace of bedding on an intersecting foliation plane commonly appears as color stripes generally parallel to local fold axes hence it is sometimes called strip ing lineation. Foliation and lineation, related to non coaxial strain shearing.
Origin of striping lineation and transposition of linear. Lstectonite balanced combination of foliation sfabric and a penetrative fabric l. The origin of foliation and lineation in the onaping. Ppt foliation and lineation powerpoint presentation. For centuries, however, manuscript curators have been numbering the recto of each leaf to facilitate study and conservation. S0, s 1, s 2 multiple planar fabrics ordered by number of relative age lineation fabric elements are linear. Distinguish foliation in geology refers to repetitive layering in metamorphic rocks.
Certain minerals, most notably the mica group, are mostly thin and planar by default. A lineation defined by the hinges of small folds crenulations associated with crenulation cleavage. A penetrative secondary foliation and lineation, defined by tectonically flattened and elongated fragments, are present in the onaping formation of the south and east ranges of the sudbury basin. It is caused by shearing forces pressures pushing different sections of the rock in different. Difference between foliation and layering difference between. In this paper, the notion of a distribution will be presented which makes it possible for in. Nordkalott project, 1986 in southwestern sweden, the residuals show a northsouth trend compared with the nesw. Foliation and lineation are two separate entities, but are often found complementing one another in the same metamorphic rocks, as you will see later. Lineation only, due to unidirectional stretching or constriction. Geology foliation and lineation symbols geonet, the esri. Geological background, rock mechanics significance, and preliminary investigations at olkiluoto abstract a well developed, pervasive foliation is a characteristic feature of the migmatites and gneisses in the olkiluoto bedrock, and.
A pictorial guide to metamorphic rocks in the field. Two nonparallel foliations can also produce an i ntersection lineation. Foliation is common to rocks affected by regional metamorphic compression typical of orogenic belts. Foliation development and refraction in metamorphic rocks. Two nonparallel foliations can also produce an intersection lineation. A new method, following crystallographic terminology, of describing lineation in gneisses, which do not possess foliation. Bedding in a sedimentary rock and magmatic layering in igneous rocks are the most. Foliation definition of foliation by merriamwebster. Crenulation lineation is almost always visible when crenulation cleavage is present. These elements formed not by shearing, as previously supposed, but by flowage such that maximum shortening was normal to the foliation and maximum. Its eventual goal is to describe the classifying space for codlmenslon g foliated manifolds which has recently been constructed by. Lineation the word lineation is used to describe any linear structure that. Ppt foliation and lineation powerpoint presentation free.
Rocks that are pervaded by foliation andor lineation flowed in solid state. Foliations, lineations and lattice preferred orientation. Near where i live there is a metaconglomerate where the individual clasts are 2cm wide and thick, but up to 100cm long. The stretching lineation in a reactivated foliation can be radically reoriented, potentially causing major errors in determining movement directions in mylonitic schistosities in folded thrusts. The term unfoliated gneiss is coined to describe such gneissic rocks with lineation alone and without. A much more rare texture type with 100 poles perpendicular to the foliation and 001 parallel to the lineation fig.
451 684 1279 875 180 1607 523 1181 1385 707 172 1613 182 1044 788 971 1232 20 1505 1336 66 1420 642 759 1616 479 1456 534 1428 156 528 996