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Igneous Rocks by Joseph Paxson Iddings

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1Petrology Of The Igneous Rocks

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2A Descriptive Petrography Of The Igneous Rocks

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3Unearthing Igneous Rocks

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4Report On The Copper Deposits Of The Eastern Townships Of Quebec With A Review Of The Igneous Rocks Of The District [microform]

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5Recent Advances In The Geology Of Igneous Rocks

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6Origins Of Igneous Rocks

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7On The Existence Of Phosphoric Acid In Rocks Of Igneous Origin.

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On the Existence of Phosphoric Acid in Rocks of Igneous origin. Fownes, G Abstracts of the Papers Communicated to the Royal Society of London (1843-1854). 1843-01-01. 5:508–509

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8British Petrography With Special Reference To The Igneous Rocks

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On the Existence of Phosphoric Acid in Rocks of Igneous origin. Fownes, G Abstracts of the Papers Communicated to the Royal Society of London (1843-1854). 1843-01-01. 5:508–509

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9NASA Technical Reports Server (NTRS) 19930000964: Thermobarometric Studies On The Levack Gneisses: Footwall Rocks To The Sudbury Igneous Complex

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Granulite and amphibolite facies gneisses and migmatites of the Levack Gneiss Complex occupy a zone up to 8 km wide around the northern part of the Sudbury Igneous Complex (SIC). Orthopyroxene- and garnet-bearing tonalitic and semipelitic assemblages of granulite facies grade occur within 3 km of the SIC together with lenses of mafic and pyroxenitic rock compositions normally represented by an amphibole +/- cpx-rich assemblage; amphibolite facies assemblages dominate elsewhere in this terrain. These 2.711-Ga gneisses were introduced by (1) the Cartier Granite Batholith during late Archaean to early Proterozoic time and (2) the SIC, at 1.85 Ga, which produced a contact aureole 1-1.5 km wide in which pyroxene hornfelses are common within 200-300 m of the contact. A suite of 12 samples including both the opx-gt and amphibole-rich rock compositions have been studied. Garnets in the semipelitic gneisses are variably replaced by a plg-bio assemblage. Thermobarometric calculations using a variety of barometers and thermometers reported in the literature suggest that the granulite facies assemblages formed at depths in the 21-28 km range (6-8 kbar). Textures and mineral chemistry in the garnet-bearing semipelitic rocks indicate that this terrain underwent a second metamorphic event during uplift to depth in the 5-11 km range (2-3 kbar) and at temperatures as low as 500-550 C. This latter event is distinct from thermal recrystallization caused by the emplacement of the SIC; it probably represents metamorphism attributable to intrusion of the Cartier Granite Batholith. These data allow two interpretations for the crustal uplift of the Levack Gneisses: (1) The gneisses were tectonically uplifted prior to the Sudbury Event (due to intrusion of the Cartier Batholith); or (2) the gneisses were raised to epizonal levels as a result of meteorite impact at 1.85 Ga.

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10NASA Technical Reports Server (NTRS) 19770015090: Introduction To The Apollo Collections. Part 1: Lunar Igneous Rocks

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The basic petrographic, chemical, and age data is presented for a representative suite of igneous rocks gathered during the six Apollo missions. Tables are given for 69 samples: 32 igneous rocks and 37 impactites (breccias). A description is given of 26 basalts, four plutonic rocks, and two pyroclastic samples. The textural-mineralogic name assigned each sample is included.

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11Charge Generation And Propagation In Igneous Rocks

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Various electrical phenomena have been reported prior to or concurrent with earthquakes such as resistivity changes, ground potentials, electromagnetic (EM), and luminous signals. Doubts have been raised as to whether some of these phenomena are real and indeed precursory. One of the reasons for uncertainty is that, despite decades of intense work, there is still no physically coherent model. Using low- to medium-velocity impacts to measure electrical signals with microsecond time resolution, it has now been observed that when dry gabbro and diorite cores are impacted at relatively low velocities, approximately 100 m/s, highly mobile charge carriers are generated in a small volume near the impact point. They spread through the rocks, causing electric potentials exceeding 400 mV, EM, and light emission. As the charge cloud spreads, the rock becomes momentarily conductive. When a dry granite block is impacted at higher velocity, approximately 1.5 km/s, the propagation of the P and S waves is registered through the transient piezoelectric response of quartz. After the sound waves have passed, the surface of the granite block becomes positively charged, suggesting the same charge carriers as observed during the low-velocity impact experiments, expanding from within the bulk. During the next 2-3 ms the surface potential oscillates, indicating pulses of electrons injected from ground and contact electrodes. The observations are consistent with positive holes, e.g., defect electrons in the O(2-) sublattice, traveling via the O 2p-dominated valence band of the silicate minerals. Before activation, the positive holes lay dormant in the form of electrically inactive positive hole pairs (PHP), chemically equivalent to peroxy links, O3X/OO\XO3, with X=Si(4), Al(3), etc. PHPs are introduced into the minerals by way of hydroxyl,O3X-OH, which all nominally anhydrous minerals incorporate when crystallizing in H2O-laden environments. The fact that positive holes can be activated by low-energy impacts, and their attendant sound waves, suggests that they can also be activated by microfracturing. Depending on where in the stressed rock volume the charge carriers are activated, they will form rapidly moving or fluctuating charge clouds that may account for earthquake-related electrical signals and EM emission. Wherever such charge clouds intersect the surface, high fields are expected, causing electric discharges and earthquake lights.

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12The Evolution Of The Igneous Rocks

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Various electrical phenomena have been reported prior to or concurrent with earthquakes such as resistivity changes, ground potentials, electromagnetic (EM), and luminous signals. Doubts have been raised as to whether some of these phenomena are real and indeed precursory. One of the reasons for uncertainty is that, despite decades of intense work, there is still no physically coherent model. Using low- to medium-velocity impacts to measure electrical signals with microsecond time resolution, it has now been observed that when dry gabbro and diorite cores are impacted at relatively low velocities, approximately 100 m/s, highly mobile charge carriers are generated in a small volume near the impact point. They spread through the rocks, causing electric potentials exceeding 400 mV, EM, and light emission. As the charge cloud spreads, the rock becomes momentarily conductive. When a dry granite block is impacted at higher velocity, approximately 1.5 km/s, the propagation of the P and S waves is registered through the transient piezoelectric response of quartz. After the sound waves have passed, the surface of the granite block becomes positively charged, suggesting the same charge carriers as observed during the low-velocity impact experiments, expanding from within the bulk. During the next 2-3 ms the surface potential oscillates, indicating pulses of electrons injected from ground and contact electrodes. The observations are consistent with positive holes, e.g., defect electrons in the O(2-) sublattice, traveling via the O 2p-dominated valence band of the silicate minerals. Before activation, the positive holes lay dormant in the form of electrically inactive positive hole pairs (PHP), chemically equivalent to peroxy links, O3X/OO\XO3, with X=Si(4), Al(3), etc. PHPs are introduced into the minerals by way of hydroxyl,O3X-OH, which all nominally anhydrous minerals incorporate when crystallizing in H2O-laden environments. The fact that positive holes can be activated by low-energy impacts, and their attendant sound waves, suggests that they can also be activated by microfracturing. Depending on where in the stressed rock volume the charge carriers are activated, they will form rapidly moving or fluctuating charge clouds that may account for earthquake-related electrical signals and EM emission. Wherever such charge clouds intersect the surface, high fields are expected, causing electric discharges and earthquake lights.

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13The Manhattan Schist Of Southeastern New York State And Its Associated Igneous Rocks

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Fettke, Charles R. The Manhattan schist of southeastern New York State and its associated igneous rocks [s. n.] , New York : 1914. 193-260 p., 8 leaves of plates : ill., map (fold.) ; 24 cm. Contributions from the Department of Geology of Columbia University, vol. XXVI ; no. 4

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14Classification Of Igneous Rocks

"Classification of Igneous Rocks" is an article from The American Naturalist, Volume 32 . View more articles from The American Naturalist . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-2454512

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15Igneous And Metamorphic Rocks Of Parts Of Sequoia And Kings Canyon National Parks, California

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Bibliography: p. 23-24

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16Two Types Of Tourmaline With Igneous And Metamorphic Origin In Metamorphic Rocks Of North Golpayegan, Isfahan Province

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The Muteh-Golpayegan metamorphic complex consist of different metamorphic rocks including pelitic, semi-pelitic, carbonate, quartz-feldspathic and basic metamorphosed rocks. The metapelitic rocks include chlorite schist, biotite schist, garnet schist, staurolite schist, kyanite schist, sillimanite schist and andalusite schist. The semi-pelitic rocks contain higher amounts of quartz and lower amounts of mica. Apart from the main minerals in the rocks, which are quartz, muscovite, biotite, chlorite, garnet, staurolite, sillimanite, kyanite and andalusite, some samples contain considerable amounts of tourmaline as minor mineral. Tourmaline was studied in one pelitic sample and one semi-pelitic sample with high quartz content.  Tourmaline in both lithologies contain high amounts of Na+K relative to Ca in the X crystallographical site, indicating alkaline tourmalines for the studied samples. Low Ca contents points to low uvite content or limited Ca(Fe,Mg)(Na,Al)-1 substitution. The Al content is higher than 6 atoms per formula unit (6.519-6.968), making them Al-bearing tourmalines. Tourmaline in the pelitic samples is schorl, with igneous origin from detrital tourmalines in granitoids, while tourmaline in semi-pelitic sample is dravite with metamorphic origin, more likely formed during regional metamorphism in the Golpayegan area.

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17Introduction To The Study Of Igneous Rocks

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18Born Of Fire : Volcanoes And Igneous Rocks

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19Igneous Minerals And Rocks

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ix, 367 p. incl. illus., tables, diagrs. 22 cm

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20Spirit Discovers New Class Of Igneous Rocks

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During the past two-and-a-half years of traversing the central part of Gusev Crater, NASA's Mars Exploration Rover Spirit has analyzed the brushed and ground-into surfaces of multiple rocks using the alpha particle X-ray spectrometer, which measures the abundance of major chemical elements. In the process, Spirit has documented the first example of a particular kind of volcanic region on Mars known as an alkaline igneous province. The word alkaline refers to the abundance of sodium and potassium, two major rock-forming elements from the alkali metals on the left-hand side of the periodic table. All of the relatively unaltered rocks -- those least changed by wind, water, freezing, or other weathering agents -- examined by Spirit have been igneous, meaning that they crystallized from molten magmas. One way geologists classify igneous rocks is by looking at the amount of potassium and sodium relative to the amount of silica, the most abundant rock-forming mineral on Earth. In the case of volcanic rocks, the amount of silica present gives scientists clues to the kind of volcanism that occurred, while the amounts of potassium and sodium provide clues about the history of the rock. Rocks with more silica tend to erupt explosively. Higher contents of potassium and sodium, as seen in alkaline rocks like those at Gusev, may indicate partial melting of magma at higher pressure, that is, deeper in the Martian mantle. The abundance of potassium and sodium determines the kinds of minerals that make up igneous rocks. If igneous rocks have enough silica, potassium and sodium always bond with the silica to form certain minerals. The Gusev rocks define a new chemical category not previously seen on Mars, as shown in this diagram plotting alkalis versus silica, compiled by University of Tennessee geologist Harry McSween. The abbreviations "Na2O" and "K2O" refer to oxides of sodium and potassium. The abbreviation "SiO2" refers to silica. The abbreviation "wt. %" indicates that the numbers tell what percentage of the total weight of each rock is silica (on the horizontal scale) and what percentage is oxides of sodium and potassium (on the vertical scale). The thin lines separate volcanic rock types identified on Earth by different scientific names such as foidite and picrobasalt. Various classes of Gusev rocks (see box in upper right) all plot either on or to the left of the green lines, which define "alkaline" and "subalkaline" categories (subalkaline rocks have more silica than alkaline rocks). Members of the rover team have named different classes of rocks after specimens examined by Spirit that represent their overall character. During the rover's travels, Spirit discovered that Adirondack-class rocks littered the Gusev plains; that Backstay, Irvine, and Wishstone-class rocks occurred as loose blocks on the northwest slope of "Husband Hill"; and that outcrops of Algonquin-class rocks protruded in several places on the southeast face. These rocks have less silica than all previously analyzed Mars samples, which are subalkaline. The previously analyzed Mars samples include Martian meteorites found on Earth and rocks analyzed by the Mars Pathfinder rover in 1997. Gusev is the first documented example of an alkaline igneous province on Mars.

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21A Contribution To The Geology Of The Pre-Cambrian Igneous Rocks Of The Fox River Valley, Wisconsin

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22Introduction To The Study Of Igneous Rocks

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23Igneous Rocks

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24Igneous Rocks

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25Igneous Rocks

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26The Natural History Of Igneous Rocks

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27What Are Igneous Rocks?

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28The Age Of The Igneous Rocks Of Iceland

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29A Look At Igneous Rocks

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30Text-book Of Petrology, Containing A Summary Of The Modern Theories Of Petrogenesis, A Description Of The Rock-forming Minerals, And A Synopsis Of The Chief Types Of The Igneous Rocks And Their Distribution As Illustrated By The British Isles

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"General works of reference": p. xv-xvi

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31The Physical Chemistry Of The Crystallization And Magmatic Differentiation Of Igneous Rocks. II

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"The Physical Chemistry of the Crystallization and Magmatic Differentiation of Igneous Rocks. II" is an article from The Journal of Geology, Volume 29 . View more articles from The Journal of Geology . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-30080756

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32The Igneous Rocks Of Kansas

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"The Igneous Rocks of Kansas" is an article from Transactions of the Annual Meetings of the Kansas Academy of Science, Volume 8 . View more articles from Transactions of the Annual Meetings of the Kansas Academy of Science . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-3623843

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33Introduction To The Apollo Collections. Part 1, Lunar Igneous Rocks

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Basic petrographic, chemical, and age data is presented for a representative suite of igneous rocks gathered during the six Apollo missions.

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34NASA Technical Reports Server (NTRS) 20150002921: Classification Scheme For Diverse Sedimentary And Igneous Rocks Encountered By MSL In Gale Crater

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The Curiosity Rover landed in a lithologically and geochemically diverse region of Mars. We present a recommended rock classification framework based on terrestrial schemes, and adapted for the imaging and analytical capabilities of MSL as well as for rock types distinctive to Mars (e.g., high Fe sediments). After interpreting rock origin from textures, i.e., sedimentary (clastic, bedded), igneous (porphyritic, glassy), or unknown, the overall classification procedure (Fig 1) involves: (1) the characterization of rock type according to grain size and texture; (2) the assignment of geochemical modifiers according to Figs 3 and 4; and if applicable, in depth study of (3) mineralogy and (4) geologic/stratigraphic context. Sedimentary rock types are assigned by measuring grains in the best available resolution image (Table 1) and classifying according to the coarsest resolvable grains as conglomerate/breccia, (coarse, medium, or fine) sandstone, silt-stone, or mudstone. If grains are not resolvable in MAHLI images, grains in the rock are assumed to be silt sized or smaller than surface dust particles. Rocks with low color contrast contrast between grains (e.g., Dismal Lakes, sol 304) are classified according to minimum size of apparent grains from surface roughness or shadows outlining apparent grains. Igneous rocks are described as intrusive or extrusive depending on crystal size and fabric. Igneous textures may be described as granular, porphyritic, phaneritic, aphyric, or glassy depending on crystal size. Further descriptors may include terms such as vesicular or cumulate textures.

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35Platinum And Palladium In Mafic-ultramafic Igneous Rocks, Northwestern Alaska

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The Curiosity Rover landed in a lithologically and geochemically diverse region of Mars. We present a recommended rock classification framework based on terrestrial schemes, and adapted for the imaging and analytical capabilities of MSL as well as for rock types distinctive to Mars (e.g., high Fe sediments). After interpreting rock origin from textures, i.e., sedimentary (clastic, bedded), igneous (porphyritic, glassy), or unknown, the overall classification procedure (Fig 1) involves: (1) the characterization of rock type according to grain size and texture; (2) the assignment of geochemical modifiers according to Figs 3 and 4; and if applicable, in depth study of (3) mineralogy and (4) geologic/stratigraphic context. Sedimentary rock types are assigned by measuring grains in the best available resolution image (Table 1) and classifying according to the coarsest resolvable grains as conglomerate/breccia, (coarse, medium, or fine) sandstone, silt-stone, or mudstone. If grains are not resolvable in MAHLI images, grains in the rock are assumed to be silt sized or smaller than surface dust particles. Rocks with low color contrast contrast between grains (e.g., Dismal Lakes, sol 304) are classified according to minimum size of apparent grains from surface roughness or shadows outlining apparent grains. Igneous rocks are described as intrusive or extrusive depending on crystal size and fabric. Igneous textures may be described as granular, porphyritic, phaneritic, aphyric, or glassy depending on crystal size. Further descriptors may include terms such as vesicular or cumulate textures.

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36Modifications Of The "Quantitative System Of Classification Of Igneous Rocks"

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"Modifications of the "Quantitative System of Classification of Igneous Rocks"" is an article from The Journal of Geology, Volume 20 . View more articles from The Journal of Geology . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-30061100

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37A Descriptive Petrography Of The Igneous Rocks

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38The Age And Succession Of The Igneous Rocks Of The Sierra Nevada

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"The Age and Succession of the Igneous Rocks of the Sierra Nevada" is an article from The Journal of Geology, Volume 3 . View more articles from The Journal of Geology . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-30055058

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39The Order Of Crystallization In Igneous Rocks

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"The Order of Crystallization in Igneous Rocks" is an article from The Journal of Geology, Volume 20 . View more articles from The Journal of Geology . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-30060758

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40The Average Chemical Composition Of Igneous Rocks

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"The Average Chemical Composition of Igneous Rocks" is an article from Proceedings of the National Academy of Sciences of the United States of America, Volume 8 . View more articles from Proceedings of the National Academy of Sciences of the United States of America . View this article on JSTOR . View this article's JSTOR metadata . You may also retrieve all of this items metadata in JSON at the following URL: https://archive.org/metadata/jstor-84389

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41Igneous Rocks A Classification And Gloss

Geochemistry

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42Igneous Rocks

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Geochemistry

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43Igneous Rocks

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Geochemistry

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44Igneous Rocks; Composition, Texture And Classification, Description And Occurrance

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Geochemistry

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45Igneous Rocks And Iron Ores Of Kiirunavaara, Luossavaara And Tuolluvaara

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Bibliography: p. 274-278

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46Granite And Other Igneous Rocks

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Bibliography: p. 274-278

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47Igneous Rocks

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Bibliography: p. 274-278

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48Trace Elements, Rare Earths, And Chemical Composition Of Southern Illinois Igneous Rocks

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Bibliography: p. 274-278

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49The Tertiary Igneous Rocks Of Skye

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Bibliography: p. 274-278

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50Petrography And Geology Of The Igneous Rocks Of The Highwood Mountains, Montana

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Book digitized by Google from the library of Harvard University and uploaded to the Internet Archive by user tpb.

“Petrography And Geology Of The Igneous Rocks Of The Highwood Mountains, Montana” Metadata:

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1Igneous rocks

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Book's cover

“Igneous rocks” Metadata:

  • Title: Igneous rocks
  • Author:
  • Language: English
  • Number of Pages: Median: 465
  • Publisher: ➤  John Wiley & Sons - J. Wiley & Sons - J. Wiley & sons; [etc., etc.]
  • Publish Date:
  • Publish Location: New York

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  • First Year Published: 1909
  • Is Full Text Available: Yes
  • Is The Book Public: Yes
  • Access Status: Public

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    2Igneous Rocks: Composition, Texture and Classification, Description and Occurrance

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    Book's cover

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    • Title: ➤  Igneous Rocks: Composition, Texture and Classification, Description and Occurrance
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    • Number of Pages: Median: 507
    • Publisher: J. Wiley & sons; [etc ., etc.]
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    “Igneous Rocks: Composition, Texture and Classification, Description and Occurrance” Subjects and Themes:

    Edition Identifiers:

    • The Open Library ID: OL20511861M
    • Online Computer Library Center (OCLC) ID: 304458
    • Library of Congress Control Number (LCCN): 09015884

    Access and General Info:

    • First Year Published: 1909
    • Is Full Text Available: Yes
    • Is The Book Public: Yes
    • Access Status: Public

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      3The mineral composition and geological occurrence of certain igneous rocks in the Yellowstone National Park

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      Book's cover

      “The mineral composition and geological occurrence of certain igneous rocks in the Yellowstone National Park” Metadata:

      • Title: ➤  The mineral composition and geological occurrence of certain igneous rocks in the Yellowstone National Park
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      • Language: English
      • Number of Pages: Median: 200
      • Publisher: ➤  Philosophical Society of Washington
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      • Publish Location: Washington, D.C

      “The mineral composition and geological occurrence of certain igneous rocks in the Yellowstone National Park” Subjects and Themes:

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      • First Year Published: 1890
      • Is Full Text Available: Yes
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        4Quantitative classification of igneous rocks

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        “Quantitative classification of igneous rocks” Metadata:

        • Title: ➤  Quantitative classification of igneous rocks
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        • Language: English
        • Number of Pages: Median: 315
        • Publisher: ➤  Creative Media Partners, LLC - W. Wesley
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        • First Year Published: 1902
        • Is Full Text Available: Yes
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          5Quantitative classification of igneous rocks

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          “Quantitative classification of igneous rocks” Metadata:

          • Title: ➤  Quantitative classification of igneous rocks
          • Authors:
          • Language: English
          • Number of Pages: Median: 286
          • Publisher: ➤  The University of Chicago Press - W. Wesley & Son
          • Publish Date:
          • Publish Location: London - Chicago

          “Quantitative classification of igneous rocks” Subjects and Themes:

          Edition Identifiers:

          • The Open Library ID: OL6923145M
          • Online Computer Library Center (OCLC) ID: 3557318
          • Library of Congress Control Number (LCCN): 03000584

          Access and General Info:

          • First Year Published: 1903
          • Is Full Text Available: Yes
          • Is The Book Public: Yes
          • Access Status: Public

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