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Journal articles on the topic 'Clastic dyke'

Author: Grafiati

Published: 4 June 2021

Last updated: 19 February 2022

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1

CURTIS, MICHAEL L., and TEAL R. RILEY. "Mobilization of fluidized sediment during sill emplacement, western Dronning Maud Land, East Antarctica." Antarctic Science 15, no. 3 (2003): 393–98. http://dx.doi.org/10.1017/s0954102003001408.

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Large mafic sills in the Ahlmannryggen region of western Dronning Maud Land were intruded into partially lithified sediments of the mid-Proterozoic Ritscherflya Supergroup. Clastic sedimentary dykes intruding the thick mafic sills have been identified, and show evidence for fluidization of the partially lithified sediments. Previous work had demonstrated in situ fluidization and localized anatectic melting. This study demonstrates mobilization of the fluidized sediments, with penetration at least 50 m into the fractured, intruding sill. Physical features within the clastic dykes (e.g. sediment

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2

Chown, E. H., and André Gobeil. "Clastic dykes of the Chibougamau Formation: distribution and origin." Canadian Journal of Earth Sciences 27, no. 8 (1990): 1111–14. http://dx.doi.org/10.1139/e90-115.

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Undeformed clastic dykes cut Archean crystalline rocks in two northeast-trending zones west of Chibougamau, Quebec. The dykes contain varying amounts of granule- to pebble-sized lithic fragments in a fine-grained matrix of angular mineral clasts, identical to material composing the nearby Lower Proterozoic Chibougamau Formation. This extends the area known to have been covered by the Chibougamau Formation more than 80 km to the west. Dyke structures suggest forceful downward intrusion of water-laden sediment, related to either syn- or postsedimentary fault movements.

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3

Le Heron, Daniel Paul, and James L. Etienne. "A complex subglacial clastic dyke swarm, Sólheimajökull, southern Iceland." Sedimentary Geology 181, no. 1-2 (2005): 25–37. http://dx.doi.org/10.1016/j.sedgeo.2005.06.012.

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4

Chown, E. H., and Guy Archambault. "The transition from dyke to sill in the Otish Mountains, Quebec; relations to host-rock characteristics." Canadian Journal of Earth Sciences 24, no. 1 (1987): 110–16. http://dx.doi.org/10.1139/e87-009.

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The Otish gabbro sills intrude Aphebian clastic rocks lying uncanformably on the Archean rocks of the Superior Province close to its juncture with the Grenville Province. The sills are undated but by inference may be ca. 1750 Ma. Two dyke swarms are known in the vicinity, the 1950 Ma, northwest-trending Mistassini dykes and a northeast-trending swarm of unknown age extending 600 km from Senneterre to the Otish Mountains and possibly another 300 km to the northeast. The trends of feeder dykes to the Otish sills are physically compatible with the dominant northeast dykes, which are therefore con

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Sach, Volker J., Elmar Buchner, and Martin Schmieder. "Enigmatic earthquake-generated large-scale clastic dyke in the Biberach area (SW Germany)." Sedimentary Geology 398 (March 2020): 105571. http://dx.doi.org/10.1016/j.sedgeo.2019.105571.

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6

Boulter, C. A. "Accretionary lapilli-filled clastic dykes: a comparison of compaction strain estimates from dyke folding and lapilli shape factors." Journal of Structural Geology 8, no. 2 (1986): 201–4. http://dx.doi.org/10.1016/0191-8141(86)90110-0.

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7

Friderichsen, J. D., and H. J. Bengaard. "The North Greenland fold belt in eastern Nansen Land." Rapport Grønlands Geologiske Undersøgelse 126 (December 31, 1985): 69–78. http://dx.doi.org/10.34194/rapggu.v126.7912.

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Field work in 1984 shows that Nansen Land consists of clastic rocks of the carbonaceous Paradisfjeld Group and terrigeneous rocks of the Polkorridoren Group; both are lower Cambrian in age and deposited in a slope and fan environment. Two major Ellesmerian (Devonian to Carboniferous) phases of deformation gave rise to east-west trending folds and schistosities. Three phases of Eurekan (upper Cretaceous to Tertiary) deformation, associated with dyke intrusion, are recognised. The second of these may be related to transpression on the Harder Fjord fault zone, though no major strike-slip movement

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8

Goździk, Jan, and Antonius J. (Tom) van Loon. "The origin of a giant downward directed clastic dyke in a kame (Bełchatów mine, central Poland)." Sedimentary Geology 193, no. 1-4 (2007): 71–79. http://dx.doi.org/10.1016/j.sedgeo.2006.02.008.

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9

NATAL’IN, BORIS, and ADALET GIZEM SAY. "Eocene–Oligocene stratigraphy and structural history of the Karaburun area, southwestern Black Sea coast, Turkey: transition from extension to compression." Geological Magazine 152, no. 6 (2015): 1104–22. http://dx.doi.org/10.1017/s0016756815000229.

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AbstractThe stratigraphic succession exposed in the Karaburun area (southern Black Sea coast, NW Turkey) records multiple changes in depositional and tectonic settings during Cenozoic times. It starts with the Middle–Upper Eocene Soğucak Formation of reef limestone that across a normal fault, omitting the lower part of the Lower Oligocene Ceylan Formation (deep-marine shale unit), abuts the upper part of the Ceylan Formation that is made up of two facies: (1) shallow-marine sandstone and (2) shallow-marine limestone units containing horizons of submarine slumps. Both facies are unconformably o

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10

Blein, Olivier, Henriette Lapierre, Richard A. Schweickert, Arnaud Pecher, and Cedric Reynaud. "Volcanisme triasique calco-alcalin a shoshonitique du Nevada occidental." Bulletin de la Société Géologique de France 172, no. 2 (2001): 189–200. http://dx.doi.org/10.2113/172.2.189.

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Abstract Two types of island-arc occur in the North American Cordillera during the Permian-Triassic times. The first type is exposed in the eastern Klamath and Blue Mountains (fig. 1). Its stratigraphy is continuous from Permian to Triassic, and is composed of arc-tholeiites with minor calc-alkaline lavas. This suite shows high epsilon Nd (sub (T)) values similar to the range of intra-oceanic island-arc [Lapierre et al., 1987; Brouxel et al., 1987, 1988; Charvet et al., 1990; Lapierre et al., 1990, 1994]. In contrast, the second type, exposed in northern Sierra Nevada and central-western Nevad

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11

Coetzee, A., and A. F. M. Kisters. "Spatial variations of sills and implications for magma dispersal across the Karoo basin." South African Journal of Geology 123, no. 4 (2020): 511–30. http://dx.doi.org/10.25131/sajg.123.0035.

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Abstract Dolerite sill complexes of the Karoo Large Igneous Province (ca. 183 Ma) show systematic variations in emplacement style and size throughout the Karoo basin. These variations are explained in terms of three main, interrelated factors, namely the overburden thickness or emplacement depth, variations in host rock rigidities as a result of sedimentary facies changes in the Karoo basin, and proximity to magma feeders. In the northern parts of the thinner (&lt;500 m) and more coarse-clastic Karoo stratigraphy, sills intrude preferentially below more rigid sandstone horizons that acted

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12

Shaw, CSJ, G. M. Young, and C. M. Fedo. "Sudbury-type breccias in the Huronian Gowganda Formation near Whitefish Falls, Ontario: products of diabase intrusion into incompletely consolidated sediments?" Canadian Journal of Earth Sciences 36, no. 9 (1999): 1435–48. http://dx.doi.org/10.1139/e99-057.

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Sudbury breccias are commonly attributed to meteoritic impact at about 1.85 Ga in the vicinity of the Sudbury Igneous Complex. In the Whitefish Falls area, about 75 km southwest of Sudbury, similar breccias are widely developed in argillites of the ~2.3 Ga Gowganda Formation. There is abundant evidence of "soft sediment" deformation of the Huronian sediments in the form of complex "fault" contacts, clastic dyke intrusions, and chaotic folding. These movements appear to have been penecontemporaneous with intrusion of highly irregular diabase bodies, which are interpreted as being older than the

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13

Embry, Ashton F., and Kirk G. Osadetz. "Stratigraphy and tectonic significance of Cretaceous volcanism in the Queen Elizabeth Islands, Canadian Arctic Archipelago." Canadian Journal of Earth Sciences 25, no. 8 (1988): 1209–19. http://dx.doi.org/10.1139/e88-118.

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Cretaceous volcanic rocks, which consist mainly of basalt flows and pyroclastic rocks, occur on northern Ellesmere Island, Axel Heiberg Island, and northernmost Amund Ringnes Island as part of the Sverdrup Basin succession. Volcanic rocks are associated with each of four regional transgressive–regressive (T–R) cycles that constitute the Cretaceous clastic succession of Sverdrup Basin and are of Valanginian – early Barremian, late Barremian – Aptian, latest Aptian – early Cenomanian, and late Cenomanian – Maastrichtian age; the volcanic component of each increases northward. The centre of volca

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14

Jelsma, H. A., R. W. Nesbitt, and C. M. Fanning. "Exploring our current understanding of the geological evolution and mineral endowment of the Zimbabwe Craton." South African Journal of Geology 124, no. 1 (2021): 279–310. http://dx.doi.org/10.25131/sajg.124.0020.

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Abstract A.M. Macgregor (1888-1961) is remembered for his enormous contribution to geology. His maps changed the course of geological thinking in southern Africa. Following in his footsteps we examine aspects of our current understanding of the geological evolution of the Zimbabwe Craton and, using new SHRIMP U-Pb ages of zircons from felsic volcanic and plutonic rocks from northern Zimbabwe and unpublished data related to the seminal paper by Wilson et al. (1995), a synthesis is proposed for the formation of the Neoarchaean greenstones. The data suggest marked differences (lithostratigraphy,

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15

Liu, Wei, Xiaoyong Yang, Shengyuan Shu, Lei Liu, and Sihua Yuan. "Precambrian Basement and Late Paleoproterozoic to Mesoproterozoic Tectonic Evolution of the SW Yangtze Block, South China: Constraints from Zircon U–Pb Dating and Hf Isotopes." Minerals 8, no. 8 (2018): 333. http://dx.doi.org/10.3390/min8080333.

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Zircon U–Pb dating and Hf isotopic analyses are performed on clastic rocks, sedimentary tuff of the Dongchuan Group (DCG), and a diabase, which is an intrusive body from the base of DCG in the SW Yangtze Block. The results provide new constraints on the Precambrian basement and the Late Paleoproterozoic to Mesoproterozoic tectonic evolution of the SW Yangtze Block, South China. DCG has been divided into four formations from the bottom to the top: Yinmin, Luoxue, Heishan, and Qinglongshan. The Yinmin Formation, which represents the oldest rock unit of DCG, was intruded by a diabase dyke. The ol

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16

Williamson, I. T., and B. R. Bell. "The Palaeocene lava field of west-central Skye, Scotland: Stratigraphy, palaeogeography and structure." Transactions of the Royal Society of Edinburgh: Earth Sciences 85, no. 1 (1994): 39–75. http://dx.doi.org/10.1017/s0263593300006301.

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ABSTRACTPalaeocene volcanic activity is represented in west-central Skye, Inner Hebrides, Scotland, by a laterally extensive and thick pile of sub-aerial lavas mainly belonging to the alkali olivine basalt—hawaiite—mugearite—benmoreite—trachyte suite. The lavas are typical of many continental flood basalt suites and were principally fed from fissure eruptions similar to those of present day Iceland. Intercalated with the lavas are rare beds of heterogeneous volcaniclastic material, including breccias, conglomerates, sandstones and mudstones. The sequence forms a major portion of a larger volca

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17

Dawes, P. R., N. J. Soper, J. C. Escher, and R. P. Hall. "The northern boundary of the Proterozoic (Nagssugtoqidian) mobile belt of South-East Greenland." Rapport Grønlands Geologiske Undersøgelse 146 (December 31, 1989): 54–65. http://dx.doi.org/10.34194/rapggu.v146.8097.

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The Proterozoic mobile belt of South-East Greenland has been regarded as a classic example of amphibolite facies reworking of an Archaean granulite facies gneiss terrain. Its northern boundary has been interpreted as a transcurrent shear zone in which reworking was associated with major basic dyke emplacement. A re-examination of the northern boundary shows it to be a diffuse region more than 50 km wide in which retrogression, unrelated to dykes or shear zones, gradually intensifies southwards. Superimposed on this are discrete belts of retrogression associated with dykes and shear zones. The

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18

van der Meer, Jaap J. M., K. H. Kjær, J. Krüger, J. Rabassa, and A. A. Kilfeather. "Under pressure: clastic dykes in glacial settings." Quaternary Science Reviews 28, no. 7-8 (2009): 708–20. http://dx.doi.org/10.1016/j.quascirev.2008.07.017.

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19

Ekoko Eric, Bokanda, Ekomane Emile, Eyong John Takem, et al. "Genesis of Clastic Dykes and Soft-Sediment Deformation Structures in the Mamfe Basin, South-West Region, Cameroon: Field Geology Approach." Journal of Geological Research 2018 (February 6, 2018): 1–8. http://dx.doi.org/10.1155/2018/3749725.

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This paper aims to investigate the genesis of clastic dykes and soft-sediment deformation structures in the Mamfe Basin, South West-Region, Cameroon. Results from this study portray the following: (1) The clastic dykes are extrusive and were generated from preexisting soft-sediments that penetrate fissures caused by seismic activity. It can be concluded that clastic dykes originate from seismic shacking, probably induced by volcanic-tectonic activity and magmatic dykes that cut across the Precambrian and Cretaceous formations of the Mamfe Basin. (2) The soft-sediment deformation structures (fl

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20

Fitzsimons, Sean J., and Eric A. Colhoun. "Pleistocene clastic dykes in the King Valley, western Tasmania." Australian Journal of Earth Sciences 36, no. 3 (1989): 351–63. http://dx.doi.org/10.1080/08120098908729494.

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21

Parize, O., and G. Friès. "The Vocontian clastic dykes and sills: a geometric model." Geological Society, London, Special Publications 216, no. 1 (2003): 51–72. http://dx.doi.org/10.1144/gsl.sp.2003.216.01.05.

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22

Jonk, R., J. Kelly, and J. Parnell. "The origin and tectonic significance of Lewisian- and Torridonian-hosted clastic dykes near Gairloch, NW Scotland." Scottish Journal of Geology 40, no. 2 (2004): 123–30. http://dx.doi.org/10.1144/sjg40020123.

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SynopsisA field and petrographic study of Lewisian- and Torridonian-hosted clastic dykes near Gairloch, NW Scotland indicates that these generally trend NE and align in an up to 1 km wide NE trending fracture zone extending over a distance of approximately 10 km. Clastic dykes are not pure opening mode fractures, but possess a component of horizontal shear displacement (strike-slip) as well. Margins of dykes are sharp and unaltered and clasts of lithified, host sandstones are found within those dykes hosted by the Diabaig and Applecross Formations sandstones. This suggests that fracturing and

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23

Jolly, R. J. H., J. W. Cosgrove, and D. N. Dewhurst. "Thickness and spatial distributions of clastic dykes, northwest Sacramento Valley, California." Journal of Structural Geology 20, no. 12 (1998): 1663–72. http://dx.doi.org/10.1016/s0191-8141(98)00053-4.

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24

Аlokhin, V. I., S. V. Tikhlivets, A. V. Murovska, and A. V. Puhach. "Mineralogical features of the clastic dykes of the Eastern Carpathians Skybova zone." Journal of Geology, Geography and Geoecology 27, no. 1 (2018): 3–11. http://dx.doi.org/10.15421/111824.

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We determined several areas with outcrops of clastic dikes which occur in the rocks of the Menilite suite of the Upper Paleogene period in the so-called Skybova zone [Ukr. Ски́ бова зо́на – the largest tectonic zone within the Carpathian folded structure. The word “skyba” derived from Polish, and is used in relation to nappe – Translator`s Note ] of the Eastern Carpathians. The objective of this article is to reveal the peculiarities of bedding, mineralogical composition and structural-texture peculiarities of the clastic dikes of the Sukyl, Stryi and Skhidnytsia river basins. During our resea

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Dong, Hong-Qiang, Tai-Bao Wei, Xiao-Qiang Ma, et al. "1,8-Naphthalimide-based fluorescent chemosensors: recent advances and perspectives." Journal of Materials Chemistry C 8, no. 39 (2020): 13501–29. http://dx.doi.org/10.1039/d0tc03681a.

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26

BEACOM, L. E., T. B. ANDERSON, and R. E. HOLDSWORTH. "Using basement-hosted clastic dykes as syn-rifting palaeostress indicators: an example from the basal Stoer Group, northwest Scotland." Geological Magazine 136, no. 3 (1999): 301–10. http://dx.doi.org/10.1017/s0016756899002605.

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Clastic infills of fractures (here termed clastic veins) in basement rocks immediately underlying sedimentary cover sequences can be used to date fault movements if these demonstrably occurred at the time of infilling or prior to the lithification of the entrained clastic material. This allows reconstruction of the syn-rifting palaeostress system using stress inversion techniques. During Riphean intracontinential rifting of Laurentia, the Torridonian Stoer Group sediments of northwest Scotland were deposited in half-graben basins controlled by faults, e.g. the Coigach and Clachtoll faults. At

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27

MAEKAWA, Hirokazu, Hiroya GOTO, and Masanori OKAMOTO. "Clastic dykes found in the Yakuno complex, southwest of Hyogo Prefecture, and their significance." Journal of the Geological Society of Japan 94, no. 11 (1988): 907–9. http://dx.doi.org/10.5575/geosoc.94.907.

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28

Ross, Pierre-Simon, and James D. L. White. "Unusually large clastic dykes formed by elutriation of a poorly sorted, coarser-grained source." Journal of the Geological Society 162, no. 4 (2005): 579–82. http://dx.doi.org/10.1144/0016-764904-127.

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29

Levi, Tsafrir, Ram Weinberger, Yehuda Eyal, Vladimir Lyakhovsky, and Eyal Heifetz. "Velocities and driving pressures of clay-rich sediments injected into clastic dykes during earthquakes." Geophysical Journal International 175, no. 3 (2008): 1095–107. http://dx.doi.org/10.1111/j.1365-246x.2008.03929.x.

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30

Marco, Shmuel, Ram Weinberger, and Amotz Agnon. "Radial clastic dykes formed by a salt diapir in the Dead Sea Rift, Israel." Terra Nova 14, no. 4 (2002): 288–94. http://dx.doi.org/10.1046/j.1365-3121.2002.00423.x.

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31

Rijsdijk, Kenneth F., Geraint Owen, William P. Warren, Danny McCarroll, and Jaap J. M. van der Meer. "Clastic dykes in over-consolidated tills: evidence for subglacial hydrofracturing at Killiney Bay, eastern Ireland." Sedimentary Geology 129, no. 1-2 (1999): 111–26. http://dx.doi.org/10.1016/s0037-0738(99)00093-7.

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32

Chen, Jitao, A. J. van Loon, Zuozhen Han, and S. K. Chough. "Funnel-shaped, breccia-filled clastic dykes in the Late Cambrian Chaomidian Formation (Shandong Province, China)." Sedimentary Geology 221, no. 1-4 (2009): 1–6. http://dx.doi.org/10.1016/j.sedgeo.2009.09.006.

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33

Sharma, Tarun, Nitant Shah, Lingam Gopal, et al. "Indocyanine Green Dye-Enhanced Transpupillary Thermotherapy of Classic Subfoveal Choroidal Neovascularization." Ophthalmic Surgery, Lasers and Imaging Retina 35, no. 3 (2004): 197–206. http://dx.doi.org/10.3928/1542-8877-20040501-06.

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34

Pietrzak-Renaud, Natalie J. "Sedimentary and metamorphic lithofacies of the Lower Negaunee Iron Formation, Marquette District, Michigan, USA." Canadian Journal of Earth Sciences 50, no. 12 (2013): 1165–77. http://dx.doi.org/10.1139/cjes-2012-0163.

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The base of the Proterozoic Negaunee Iron Formation is exposed in the open pit at Tilden Mine, Marquette, Michigan. Juxtaposed against the Archean-aged Palmer Gneiss, it is bounded by the regional-scale Southern Shear Zone and cut by two sets of dykes: an older chloritic and schistose set and a younger 1.1 Ga Keweenawan set. Tilden Mine is dominated by a 100 m scale plunging northwest-anticline and is cut by a growth fault locally termed the Tower Hill Fault that intersects the Southern Shear Zone. The base of the exposed iron formation is composed of three lithofacies, including lower clastic

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35

Thomas Martel, A., and Martin R. Gibling. "Clastic dykes of the Devono—Carboniferous Horton Bluff Formation, Nova Scotia: storm-related structures in shallow lakes." Sedimentary Geology 87, no. 1-2 (1993): 103–19. http://dx.doi.org/10.1016/0037-0738(93)90038-7.

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36

Chen, Jitao. "Surface and subsurface reworking by storms on a Cambrian carbonate platform: evidence from limestone breccias and conglomerates." Geologos 20, no. 1 (2014): 13–23. http://dx.doi.org/10.2478/logos-2014-0002.

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Abstract Some limestone breccias and conglomerates from the Furongian (Late Cambrian) Chaomidian Formation (Shandong Province, China) were investigated in order to understand the depositional and deformational processes induced by storms. The sediments under study occur in a hummocky cross-stratified peloidal grainstone layer. The limestone conglomerates consist of well-rounded clasts that are mostly flat-lying or imbricated, and have erosional bases. They formed by surface reworking (erosion and rip-up) of thin-bedded grainstones by storm waves and currents. The limestone breccias consist of

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37

MARTILL, DAVID M., and JOHN D. HUDSON. "Injection clastic dykes in the Lower Oxford Clay (Jurassic) of central England: relationship to compaction and concretion formation." Sedimentology 36, no. 6 (1989): 1127–33. http://dx.doi.org/10.1111/j.1365-3091.1989.tb01546.x.

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DEMOULIN, A. "Clastic dykes in east Belgium: evidence for upper Pleistocene strong earthquakes west of the Lower Rhine rift segment." Journal of the Geological Society 153, no. 5 (1996): 803–10. http://dx.doi.org/10.1144/gsjgs.153.5.0803.

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39

Szindler, Marek, Magdalena Szindler, Aleksandra Drygała, Krzysztof Lukaszkowicz, Paulina Kaim, and Rafał Pietruszka. "Dye-Sensitized Solar Cell for Building-Integrated Photovoltaic (BIPV) Applications." Materials 14, no. 13 (2021): 3743. http://dx.doi.org/10.3390/ma14133743.

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One of the important research directions in the field of photovoltaics is integration with construction. The integration of solar cell systems with a building can reduce installation costs and help optimize the used space. Among the few literature reports on photovoltaic roof tiles, solutions with silicon and thin film solar cells dominate. An interesting solution may be the application of dye-sensitized solar cells. In addition to their interesting properties, they also have aesthetic value. In the classic arrangement, they are constructed using glass with a transparent conductive layer (TCL)

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Phillips, C. A., and G. I. Alsop. "Post-tectonic clastic dykes in the Dalradian of Scotland and Ireland: implications for delayed lithification and deformation of sediments." Geological Journal 35, no. 2 (2000): 99–110. http://dx.doi.org/10.1002/1099-1034(200004/06)35:2<99::aid-gj844>3.0.co;2-x.

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41

Dulin, Shannon, R. D. Elmore, M. H. Engel, J. Parnell, and J. Kelly. "Palaeomagnetic dating of clastic dykes in Proterozoic basement, NW Scotland: evidence for syndepositional faulting during deposition of the Torridonian." Scottish Journal of Geology 41, no. 2 (2005): 149–57. http://dx.doi.org/10.1144/sjg41020149.

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42

Pešek, Jiří, and Ivana Sýkorová. "A review of the timing of coalification in the light of coal seam erosion, clastic dykes and coal clasts." International Journal of Coal Geology 66, no. 1-2 (2006): 13–34. http://dx.doi.org/10.1016/j.coal.2005.05.010.

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43

GÜRSU, S., and M. C. GÖNCÜOGLU. "Early Cambrian back-arc volcanism in the western Taurides, Turkey: implications for rifting along the northern Gondwanan margin." Geological Magazine 142, no. 5 (2005): 617–31. http://dx.doi.org/10.1017/s0016756805000919.

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The Lower Cambrian (Tommotian) Gögebakan Formation in western Central Anatolia is made up of slightly metamorphosed continental to shallow marine clastic rocks with pillowed and massive spilitic lavas and dolerite dykes. Spilitic lavas, commonly amygdaloidal, are albite- and pyroxene-phyric with the metamorphic mineral paragenesis albite+calcite+sericite±epidote±tremolite±chlorite. Dolerite dykes mainly include plagioclase and pyroxene as primary minerals and tremolite±epidote±chlorite as low-grade secondary minerals. Geochemical data show that the spilitic lavas and dolerite dykes are sub-alk

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Gibson, Alex, Wolfgang Neubauer, Sebastian Flöry, et al. "SURVEY AND SAMPLING AT THE CASTLE DYKES IRON AGE ‘HENGE’, WENSLEYDALE, NORTH YORKSHIRE." Antiquaries Journal 99 (April 15, 2019): 1–31. http://dx.doi.org/10.1017/s0003581518000628.

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Survey and sampling at the classic single-entranced henge monument at Castle Dykes, in North Yorkshire, has revealed traces of circular timber structures, interpreted as later prehistoric roundhouses, in the immediate vicinity and within the henge. Coring of the waterlogged silts of the internal ditch has produced considerable environmental data: plant, insect, pollen and charcoal remains. A small jet bead was also recovered. Radiocarbon dates from short-lived materials unexpectedly indicate that the monument was constructed in the Iron Age, which prompts a review of other potentially Iron Age

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Hill, Dominique C. "And Who Will Revere the Black Girl." Gender & Society 35, no. 4 (2021): 546–56. http://dx.doi.org/10.1177/08912432211029394.

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While the mainstream media continues to narrowly define justice and reduce the site of its presence or absence to murder scenes and court cases, justice is often foreclosed long before someone is murdered and we must #SayHerName. To expand the project of Black mattering beyond race and physical death, this essay animates how body policing through school dress code policy sanctions racial-sexual violence and provide girls with an ultimatum: either abandon body sovereignty and self-expression, or accept the consequences of being read as a distraction, a problem. (Re)membering classic Black femin

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Ribeiro, Carlos, and Pedro Terrinha. "Formation, deformation and chertification of systematic clastic dykes in a differentially lithified carbonate multilayer. SW Iberia, Algarve Basin, Lower Jurassic." Sedimentary Geology 196, no. 1-4 (2007): 201–15. http://dx.doi.org/10.1016/j.sedgeo.2006.06.001.

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Booth, Paul. "A Late Roman Military Burial from the Dyke Hills, Dorchester on Thames, Oxfordshire." Britannia 45 (July 3, 2014): 243–73. http://dx.doi.org/10.1017/s0068113x14000294.

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AbstractDamage to part of the earthwork at Dyke Hills, Dorchester on Thames, provided the opportunity to recover the badly disturbed remains of a late Roman burial which had contained an elaborate belt set and an axe. This burial, of a type very unusual in Roman Britain, is argued to be of early fifth-century date and to be directly comparable with well-known burials recovered near by in 1874 which formed a starting point for the ‘soldiers and settlers’ debates of the 1960s and beyond. The Dorchester burials are seen here as those of late Roman military personnel, and their local and wider con

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Chen, Wei, Fengting Chen, Bin Ji, Lin Zhu, and Hongjiao Song. "Insights into the mechanism of methylene blue removed by novel and classic biochars." Water Science and Technology 79, no. 8 (2019): 1561–70. http://dx.doi.org/10.2166/wst.2019.158.

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Abstract The adsorption behavior and the underlying mechanism of methylene blue (MB) sorption on biochars prepared from different feedstocks at 500 °C were evaluated. The biochar feedstocks included Magnolia grandiflora Linn. leaves biochar (MBC), pomelo (Citrus grandis) peel biochar (PBC) and badam shell biochar (BBC). The results of characterizing and analyzing the samples showed that different biochars had different effects on the adsorption of MB. It could be found that MBC had the best adsorption effect on MB due to its largest average pore diameter of 5.55 nm determined by Brunauer-Emmet

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JERRAM, DOUGAL A., KATHRYN M. GOODENOUGH, and VALENTIN R. TROLL. "Introduction: from the British Tertiary into the future – modern perspectives on the British Palaeogene and North Atlantic Igneous provinces." Geological Magazine 146, no. 3 (2009): 305–8. http://dx.doi.org/10.1017/s001675680900627x.

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The study of volcanic rocks and igneous centres has long been a classic part of geological research. Despite the lack of active volcanism, the British Isles have been a key centre for the study of igneous rocks ever since ancient lava flows and excavated igneous centres were recognized there in the 18th century (Hutton, 1788). This led to some of the earliest detailed studies of petrology. The starting point for many of these studies was the British Palaeogene Igneous Province (BPIP; formerly known as the ‘British Tertiary’ (Judd, 1889), and still recognized by this name by many geologists aro

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Marchini, Edoardo, Stefano Caramori, Carlo Alberto Bignozzi, and Stefano Carli. "On the Use of PEDOT as a Catalytic Counter Electrode Material in Dye-Sensitized Solar Cells." Applied Sciences 11, no. 9 (2021): 3795. http://dx.doi.org/10.3390/app11093795.

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Dye-sensitized solar cells (DSSCs) emerged in the early 1990s as a promising alternative to the classic silicon-based solar cell due to their unique combination of low cost, ease of fabrication, color palette for building integration, and high efficiency in indoor applications. This review article describes the fabrication and the properties of poly (3,4-ethylenedioxythiophene) (PEDOT)-based catalytic counter electrodes (CEs) for DSSCs. In particular, the electrochemical reactivity PEDOT CEs used in conjunction with alternative redox mediators for DSSCs is outlined. Among alternative redox shu

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