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Articoli di riviste sul tema "Rocks"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 25 luglio 2025

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1

Noma, Kensuke, Naotsugu Oyama, and James K. Liao. "Physiological role of ROCKs in the cardiovascular system." American Journal of Physiology-Cell Physiology 290, no. 3 (2006): C661—C668. http://dx.doi.org/10.1152/ajpcell.00459.2005.

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Rho-associated kinases (ROCKs), the immediate downstream targets of RhoA, are ubiquitously expressed serine-threonine protein kinases that are involved in diverse cellular functions, including smooth muscle contraction, actin cytoskeleton organization, cell adhesion and motility, and gene expression. Recent studies have shown that ROCKs may play a pivotal role in cardiovascular diseases such as vasospastic angina, ischemic stroke, and heart failure. Indeed, inhibition of ROCKs by statins or other selective inhibitors leads to the upregulation and activation of endothelial nitric oxide synthase

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2

Zhang, Jin Yu, Huan Sheng Dong, Reza K. Oqani, Tao Lin, Jung Won Kang, and Dong Il Jin. "Distinct roles of ROCK1 and ROCK2 during development of porcine preimplantation embryos." REPRODUCTION 148, no. 1 (2014): 99–107. http://dx.doi.org/10.1530/rep-13-0556.

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Cell-to-cell contact mediated by cell adhesion is fundamental to the compaction process that ensures blastocyst quality during embryonic development. In this study, we first showed that Rho-associated coiled-coil protein kinases (ROCK1 and ROCK2) were expressed both in porcine oocytes and IVF preimplantation embryos, playing different roles in oocytes maturation and embryo development. The amount of mRNA encoding ROCK1 and the protein concentration clearly increased between the eight-cell and morula stages, but decreased significantly when blastocysts were formed. Conversely, ROCK2 was more ab

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3

Haga, Raquel B., Ritu Garg, Francesca Collu, et al. "RhoBTB1 interacts with ROCKs and inhibits invasion." Biochemical Journal 476, no. 17 (2019): 2499–514. http://dx.doi.org/10.1042/bcj20190203.

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Abstract RhoBTB1 is an atypical Rho GTPase with two BTB domains in addition to its Rho domain. Although most Rho GTPases regulate actin cytoskeletal dynamics, RhoBTB1 is not known to affect cell shape or motility. We report that RhoBTB1 depletion increases prostate cancer cell invasion and induces elongation in Matrigel, a phenotype similar to that induced by depletion of ROCK1 and ROCK2. We demonstrate that RhoBTB1 associates with ROCK1 and ROCK2 and its association with ROCK1 is via its Rho domain. The Rho domain binds to the coiled-coil region of ROCK1 close to its kinase domain. We identif

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4

Priya, Rashmi, Xuan Liang, Jessica L. Teo, Kinga Duszyc, Alpha S. Yap, and Guillermo A. Gomez. "ROCK1 but not ROCK2 contributes to RhoA signaling and NMIIA-mediated contractility at the epithelial zonula adherens." Molecular Biology of the Cell 28, no. 1 (2017): 12–20. http://dx.doi.org/10.1091/mbc.e16-04-0262.

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Rho kinases (ROCK1 and ROCK2) function downstream of the small GTPase RhoA to drive actomyosin cytoskeletal remodeling. It has often been believed that ROCK1 and ROCK2 may be functionally redundant, as they share a highly conserved kinase domain. However, in this study, we report differential functional effects for these ROCKs at the epithelial zonula adherens (ZA). Using specific siRNA, we found that ROCK1 depletion disrupted cadherin organization at the ZA, accompanied by loss of F-actin and NMIIA, whereas ROCK2 knockdown had no significant effect. Further, ROCK1, but not ROCK2, was necessar

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5

Kitchenham, Paul. "Rock Art: “Tatooing” Rocks?" Time and Mind 2, no. 3 (2009): 347–48. http://dx.doi.org/10.2752/175169609x12464529903254.

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6

Fernández, F. J., and S. Llana-Fúnez. "Deformación asociada a la falla de Valdoviño (Noroeste del Macizo Ibérico) Deformation related to the Valdoviño fault (Northwest Iberian Massif)." Trabajos de Geología 36, no. 36 (2018): 95. http://dx.doi.org/10.17811/tdg.36.2016.95-118.

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Resumen: La sección costera de la falla de Valdoviño expone rocas de falla deformadas en las proximidades de la base de la zona sismogénica de la corteza Ibérica Varisca, en la que estructuras frágiles discretas afectan una zona de deformación predominantemente dúctil. El núcleo de la falla contiene rocas ultramáficas, rocas máficas con granate, anfibolitas, neises cuarzo-feldespáticos y metavulcanitas básicas entre las facies deformadas del granitoide Varisco de A Espenuca. Este artículo describe la deformación y microestructuras relacionadas con la falla desarrolladas en el granitoides. La c

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7

Leckie, Dale. "Petrology and tectonic significance of Gates Formation (early Cretaceous) sediments in northeast British Columbia." Canadian Journal of Earth Sciences 23, no. 2 (1986): 129–41. http://dx.doi.org/10.1139/e86-017.

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Moosebar–Gates sandstones are predominantly litharenites, with some feldspathic litharenites. Both the light- and heavy-mineral suites indicate a mixed source characterized by clastic and carbonate sedimentary rocks, acidic to intermediate plutonic and volcanic igneous rocks, and metamorphic rocks. The sediment sources all fall within a recycled orogenic provenance grouping. Histograms showing stratigraphic variation of mineral content do not indicate any significant progressive unroofing of more deeply buried source rocks.The source area was very extensive regionally and extended well into th

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8

Kravchuk, Yaroslav, Roman Hnatiuk, Myroslav Ivanyk, and Yaroslav Khomyn. "General features of relief of Marmaroshi and Pieniny rocks of Ukrainian Carpathians and their place under system of geomorphological regionalization." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 204–20. http://dx.doi.org/10.30970/vgg.2013.42.1860.

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Peculiarities of geological structure and relief of Ukrainian fragment of zones of Marmaroshi and Pieniny rocks located between Outer (Flysch) and Inner Carpathians are considered. Morphostructural differences and common features of relief of these zones are clarified. Territory of zones of Marmaroshi and Pieniny rocks is considered as separate geomorphological region of mountain part of Ukrainian Carpathians – subregion of Intermountain Valleys and Rocky Chains. Expediency of separation and taxonomic class of this geomorphological region are proved, its division into taxonomic units of lower

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9

Rahmawan, S., S. Irham, A. Nugrahanti, et al. "Carbonate Rocks Grouping Using Critical Porosity Approach in Miocene Rocks, Banggai Basin." IOP Conference Series: Earth and Environmental Science 1451, no. 1 (2025): 012011. https://doi.org/10.1088/1755-1315/1451/1/012011.

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Abstract Reservoir is the trapped location of hydrocarbons with diverse physical rock properties or high heterogeneity. The characteristics of rock heterogeneity significantly influence the rock’s ability to flow fluids, especially hydrocarbons contained within the reservoir rock. Several methods have been developed to classify the heterogeneity of reservoir rocks, such as the Amaful, Wibowo and Permadi methods, among others. These methods are developed based on experiments using sandstone rocks, although in some studies, they are also frequently employed in categorizing carbonate reservoir ro

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10

Xie, Busheng, Lixin Wu, Wenfei Mao, Shengyu Zhou, and Shanjun Liu. "An Open Integrated Rock Spectral Library (RockSL) for a Global Sharing and Matching Service." Minerals 12, no. 2 (2022): 118. http://dx.doi.org/10.3390/min12020118.

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Minerals and rocks are important natural resources that are formed over a long period of geological history. Spectroscopy is the basis of the identification and characterisation of rocks and minerals via proximal sensing in the field or remote sensing systems with multi- and hyper-spectral capabilities. However, spectral data is scattered around different institutions worldwide and stored in various formats, resulting in poor data usability and an unnecessary waste of time and information. To improve the usability and performance of mineral spectral data, we developed an integrated open minera

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Henderson, Benjamin W., Kelsey M. Greathouse, Raksha Ramdas та ін. "Pharmacologic inhibition of LIMK1 provides dendritic spine resilience against β-amyloid". Science Signaling 12, № 587 (2019): eaaw9318. http://dx.doi.org/10.1126/scisignal.aaw9318.

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Alzheimer’s disease (AD) therapies predominantly focus on β-amyloid (Aβ), but Aβ effects may be maximal before clinical symptoms appear. Downstream of Aβ, dendritic spine loss correlates most strongly with cognitive decline in AD. Rho-associated kinases (ROCK1 and ROCK2) regulate the actin cytoskeleton, and ROCK1 and ROCK2 protein abundances are increased in early AD. Here, we found that the increased abundance of ROCK1 in cultured primary rat hippocampal neurons reduced dendritic spine length through a myosin-based pathway, whereas the increased abundance of ROCK2 induced spine loss through t

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12

Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips: How Should Rocks Be Labeled?" Rocks & Minerals 63, no. 5 (1988): 407. http://dx.doi.org/10.1080/00357529.1988.11761873.

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13

Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips: Are There Rocks That Bend?" Rocks & Minerals 67, no. 3 (1992): 194–98. http://dx.doi.org/10.1080/00357529.1992.9926483.

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14

Surya Adinatha, Made Surya, and Ni Putu Tisna Andayani. "Music Creation Wajaprani | Tabuh Kreasi Wajaprani." GHURNITA: Jurnal Seni Karawitan 4, no. 2 (2024): 219–26. http://dx.doi.org/10.59997/jurnalsenikarawitan.v4i2.3409.

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Coral rocks, as an iconic element of Bali's coast, have a central role in the island's art and culture. Music, musical arts and dance in Bali often use the character and unique shapes of coral rocks found along the coast to become inspiration for works of art. In Jembrana district, precisely in Pengeragoan village, there is Yeh Leh Beach, on this beach there are beautiful coral rocks which later became the inspiration for the creation of the creative percussion work entitled Wajaprani. The rock's sturdy character even when hit by waves is an inspiration for creating dynamic rhythms. with the c

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15

Lavrskaya, Ekaterina A., Aleksey E. Selivanov, and Ksenia O. Pechenkina. "Representatives of the family Teloschistaceae as a component of the vegetation cover of rocky outcrops in the Chusovaya River valley (Middle Urals)." Вестник Пермского университета. Серия «Биология»=Bulletin of Perm University. Biology, no. 3 (2024): 263–68. http://dx.doi.org/10.17072/1994-9952-2024-3-263-268.

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The paper presents data on the patterns of lichens of the family Teloschistaceae on coastal rocks in the middle reaches of the Chusovaya River from the village of Kyn to the town of Chusovoy (Perm Krai, Sverdlovsk Oblast). To describe the lichen cover on rocky outcrops, 30×30 cm survey plots were laid out. Each site was photographed with a scale ruler, and habitat characteristics such as surface slope, exposure, overhangs, and rock were recorded. The family Teloschistaceae in the study area on rocky outcrops is represented by three genera: Caloplaca, Rusavskia, and Xanthoria. Of these genera,

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16

Md., Fahim Abrar Hossain, Tasneem Nazeefa, B. M. Rashed Alam A, and S. M. Fahad Hossain A. "Study on the Properties and Uses of Rocks Found in Bangladesh." Journal of Earthquake Science and Soil Dynamics Engineering 3, no. 3 (2020): 1–7. https://doi.org/10.5281/zenodo.4395346.

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A rock is a natural substance made up of solid crystals of various minerals that were fused into a solid lump together. The solid mineral material that is part of the earth's surface and other similar planets that is exposed on the surface or underlying the earth. There are three main rock groups: Igneous rocks, Sedimentary rocks, and Metamorphic rocks. Rocks are of great resource value like minerals, some directly, and some as mineral constituents. Nearly all types of building materials used to pave roads, floors, and house walls, or various other structures, including bridges, come from

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17

Satoh, Kimio, Yoshihiro Fukumoto, and Hiroaki Shimokawa. "Rho-kinase: important new therapeutic target in cardiovascular diseases." American Journal of Physiology-Heart and Circulatory Physiology 301, no. 2 (2011): H287—H296. http://dx.doi.org/10.1152/ajpheart.00327.2011.

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Rho-kinase (ROCKs) belongs to the family of serine/threonine kinases and is an important downstream effector of the small GTP-binding protein RhoA. There are two isoforms of Rho-kinase, ROCK1 and ROCK2, and they have different functions with ROCK1 for circulating inflammatory cells and ROCK2 for vascular smooth muscle cells. It has been demonstrated that the RhoA/Rho-kinase pathway plays an important role in various fundamental cellular functions, including contraction, motility, proliferation, and apoptosis, leading to the development of cardiovascular disease. The important role of Rho-kinas

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18

Doyle, Alexandra E., Beth Klein, Ben Zuckerman, Hilke E. Schlichting, and Edward D. Young. "Exoplanetary oxygen fugacities from polluted white dwarf stars." Proceedings of the International Astronomical Union 15, S357 (2019): 28–32. http://dx.doi.org/10.1017/s1743921320000939.

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AbstractThe intrinsic oxygen fugacity of a planet profoundly influences a variety of its geochemical and geophysical aspects. Most rocky bodies in our solar system formed with oxygen fugacities approximately five orders of magnitude higher than that corresponding to a hydrogen-rich gas of solar composition. Here we derive oxygen fugacities of extrasolar rocky bodies from the elemental abundances in 15 white dwarf (WD) stars polluted by accretion of rocks. We find that the intrinsic oxygen fugacities of rocks accreted by the WDs are similar to those of terrestrial planets and asteroids in our s

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19

Tkacz, Karolina, Filip Rolski, Marcin Czepiel, et al. "Haploinsufficient Rock1+/− and Rock2+/− Mice Are Not Protected from Cardiac Inflammation and Postinflammatory Fibrosis in Experimental Autoimmune Myocarditis." Cells 9, no. 3 (2020): 700. http://dx.doi.org/10.3390/cells9030700.

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Progressive cardiac fibrosis is a common cause of heart failure. Rho-associated, coiled-coil-containing protein kinases (ROCKs) have been shown to enhance fibrotic processes in the heart and in other organs. In this study, using wild-type, Rock1+/− and Rock2+/− haploinsufficient mice and mouse model of experimental autoimmune myocarditis (EAM) we addressed the role of ROCK1 and ROCK2 in development of myocarditis and postinflammatory fibrosis. We found that myocarditis severity was comparable in wild-type, Rock1+/− and Rock2+/− mice at day 21 of EAM. During the acute stage of the disease, hear

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20

Fagg, M. C. "Resonant Rocks, 'Rock Gongs', Idiophones And Lithophones." Geological Curator 6, no. 1 (1994): 16. http://dx.doi.org/10.55468/gc178.

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I have been studying the uses of resonant rocks, and compiling a gazetteer of'rock gongs'. These are found worldwide, and are naturally placed and naturally tuned rocks, boulders, stalagmites and stalactites, which have been used as lithophones - in contrast to other lithophones (Chinese chime stones and "barxylophones" of stone) which are artificially tuned and are portable. It is puzzling why some rocks ring and others do not.

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21

Tulkin, Annakulov, Nusratullo Ziyadov, and Farhod Abdikarimov. "Analysis of overburden transportation by conveyor transport as part of a cyclic-flow technology." E3S Web of Conferences 417 (2023): 06006. http://dx.doi.org/10.1051/e3sconf/202341706006.

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This article discusses the use of belt conveyors for transporting overburden from open pits. The main technical and economic parameters of powerful belt conveyors that operate as part of a cyclic-flow technology for the development and transportation of rocks are given. The main conclusions on the effective use and further development of belt conveyors for transporting rocky rocks are given.

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22

Zhang, Guang, Jing Xi Chen, and Bin Hu. "The Brittle-Ductile Transition Character of Rocks and Its Effect on Rockbursts." Key Engineering Materials 261-263 (April 2004): 171–76. http://dx.doi.org/10.4028/www.scientific.net/kem.261-263.171.

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The brittle-ductile character is one of the important mechanical indexes of rocks and also one of the important affecting factors of rockburst. Both conventional and true triaxial tests have shown that the brittle-ductile character of rocks varies with the variation in rocks stress state and stress path, but these two kinds of tests have revealed totally different laws of brittle-ductile transition. This present paper analyses the results from two tests firstly and then summarizes the effect of rock’s brittle-ductile transition character on rockburst and finally points out the deficiency in pr

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Lisbôa da Costa, Danúbia, Ingrid Mayara Medeiros Fernandes, Aluska Nascimento Simões Braga, Rosiane Maria da Costa Farias, Romualdo Rodrigues Menezes, and Gelmires Araújo Neves. "Microstructural Characterization of Ornamental Rock Samples: Cariri Rocks." Materials Science Forum 869 (August 2016): 159–63. http://dx.doi.org/10.4028/www.scientific.net/msf.869.159.

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Ornamental rocks are among the most promising business areas of the mineral sector, raising the necessity for, besides beauty, investments in quality, safety and characterization in the various application fields of these rocks. So, this work aims at the microstructural characterization of the class of these rocks: the Cariri Rocks, also known the limestone, which are calcareous rocks mainly formed by calcium and magnesium carbonate, possibly presenting variations due to their origins. For characterization, we studied four samples, being two from Chapada do Apodi and two from Chapada do Ararip

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Sossi, Paolo A., and Anat Shahar. "Ironing Out Isotopic Differences Among Rocky Bodies." Elements 17, no. 6 (2021): 407–12. http://dx.doi.org/10.2138/gselements.17.6.407.

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The variability of iron isotopes among rocky bodies in the inner Solar System provides a window onto the diversity of materials and mechanisms from which they formed. The magnitude of isotopic variation in mantle-derived rocks within a given body is similar to that between different planetary bodies. Isotopic signatures arising from primordial events, namely, evaporation/condensation, core formation and melting/crystallization, may be progressively diluted, modified, and redistributed over time by global recycling processes such as plate tectonics. Here, we assess the relative influence of the

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Ren, Jia Guo, and Qian Qian Wu. "Discussion on Geological Experiment Technology in Geological Work." Advanced Materials Research 616-618 (December 2012): 60–63. http://dx.doi.org/10.4028/www.scientific.net/amr.616-618.60.

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This essay puts silicate rocks test as example on the basic of the analysis of new technology and method of geological experiment. This essay analyses the experimental principal and process of silicate rock’s total iron content, and it based on geology experimental operation process. The essay tries to probe into silicate rock’s mineral chemical composition, rock structure and tectonics through the research of the iron content and other chemical components of silicate rocks. Furthermore, this essay also estimates the optional mineral’s component content of sandstone ore, and then evaluates min

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Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 60, no. 1 (1985): 36. http://dx.doi.org/10.1080/00357529.1985.11764368.

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Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 60, no. 3 (1985): 143–44. http://dx.doi.org/10.1080/00357529.1985.11764392.

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Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 60, no. 5 (1985): 245. http://dx.doi.org/10.1080/00357529.1985.11764416.

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Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 60, no. 6 (1985): 292. http://dx.doi.org/10.1080/00357529.1985.11764429.

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Titamgim, R. Dirk. "Questions and Answers about Rocks Rock Chips." Rocks & Minerals 61, no. 1 (1986): 40. http://dx.doi.org/10.1080/00357529.1986.11768433.

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Titamgim, R. Dirk. "Questions and Answers about Rocks Rock Chips." Rocks & Minerals 61, no. 2 (1986): 93–94. http://dx.doi.org/10.1080/00357529.1986.11768447.

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Titamgim, R. Dirk. "Questions and Answers about Rocks Rock Chips." Rocks & Minerals 61, no. 6 (1986): 363. http://dx.doi.org/10.1080/00357529.1986.11768471.

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Titamgim, R. Dirk. "Questions and Answers about Rocks Rock Chips." Rocks & Minerals 64, no. 3 (1989): 229–30. http://dx.doi.org/10.1080/00357529.1989.11761761.

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Titamgim, R. Dirk. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 67, no. 6 (1992): 410–15. http://dx.doi.org/10.1080/00357529.1992.9926513.

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Dietrich, R. V. "Questions and Answers about Rocks: Rock Chips." Rocks & Minerals 69, no. 2 (1994): 122–27. http://dx.doi.org/10.1080/00357529.1994.9926587.

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Dietrich, R. V. "Rock Chips Questions & Answers about Rocks." Rocks & Minerals 70, no. 5 (1995): 340–42. http://dx.doi.org/10.1080/00357529.1995.9926644.

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Dietrich, R. V. "Rock Chips: Questions & Answers about Rocks." Rocks & Minerals 71, no. 6 (1996): 412–16. http://dx.doi.org/10.1080/00357529.1996.9925634.

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Pujar, Anant G., A. Sreenivasa, and Ajaykumar N. Asode. "Petrography and Provenance Study of South-Central Part of Kaladgi Basin, Belgaum, Karnataka, India." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 108–12. http://dx.doi.org/10.46660/ijeeg.vol11.iss1.2020.421.

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Abstract (sommario):

The area under investigation covers the south-central part of Kaladgi series comprising of sedimentary rocks, mainly quartzarenites. From the geological point of view the study area comprises southcentral part of Kaladgi basin covering around 54 km2 which encompasses rocky hills of moderate height, showing three types of facies i.e., argillaceous, arenaceous and rudaceous. Among these three, arenaceous facies is more prominent in the area. These sedimentary rocks rest unconformably over gneisses. Detailed study of the rocks exposed are done by studying the petrological aspects of the rock samp

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Pujar, Anant G., A. Sreenivasa, and Ajaykumar N. Asode. "Petrography and Provenance Study of South-Central Part of Kaladgi Basin, Belgaum, Karnataka, India." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 108–12. http://dx.doi.org/10.46660/ojs.v11i1.421.

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Abstract (sommario):

The area under investigation covers the south-central part of Kaladgi series comprising of sedimentary rocks, mainly quartzarenites. From the geological point of view the study area comprises southcentral part of Kaladgi basin covering around 54 km2 which encompasses rocky hills of moderate height, showing three types of facies i.e., argillaceous, arenaceous and rudaceous. Among these three, arenaceous facies is more prominent in the area. These sedimentary rocks rest unconformably over gneisses. Detailed study of the rocks exposed are done by studying the petrological aspects of the rock samp

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Lozhnikov, O. V., V. O. Adamova, and M. M. Slivenko. "Justification of the safe parameters of recreational zones during the reclamation of watered residual quarry spaces." Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu, no. 5 (October 30, 2024): 85–92. http://dx.doi.org/10.33271/nvngu/2024-5/085.

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Purpose. To determine the safe parameters of the recreational zones created in the residual space of the quarry taking into account the physical and mechanical properties of waste rocks in a watered state. Methodology. The Bishop Simplified Method is used to determine the influence of the irrigation level of the residual quarry space on the stability of the embankment from different types of mining rocks when creating a recreational area during reclamation works. Findings. The safe parameters of recreational areas during their construction in the watered residual space of the quarry were estab

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Dietrich, R. V. "Questions and Answers about Rocks: Rock Chips: How Can I Get Others Interested in Rocks?" Rocks & Minerals 67, no. 2 (1992): 124–28. http://dx.doi.org/10.1080/00357529.1992.9926467.

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Morowitz, Harold J. "Rocks." Hospital Practice 26, no. 4 (1991): 14–17. http://dx.doi.org/10.1080/21548331.1991.11704152.

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Cooper, William E., and Wade C. Sherbrooke. "Choosing between a rock and a hard place: Camouflage in the round-tailed horned lizard Phrynosoma modestum." Current Zoology 58, no. 4 (2012): 541–48. http://dx.doi.org/10.1093/czoolo/58.4.543.

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Abstract The round-tailed horned lizard Phrynosoma modestum is cryptically colored and resembles a small stone when it draws legs close to its body and elevates its back. We investigated effectiveness of camouflage in P. modestum and its dependence on stones by placing a lizard in one of two microhabitats (uniform sand or sand with surface rocks approximately the same size as lizards). An observer who knew which microhabitat contained the lizard was asked to locate the lizard visually. Latency to detection was longer and probability of no detection within 60 s was higher for lizards on rock ba

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Harriott, Vicki J., Simon A. Banks, Roland L. Mau, Darren Richardson, and Lisa G. Roberts. "Ecological and conservation significance of the subtidal rocky reef communities of northern New South Wales, Australia." Marine and Freshwater Research 50, no. 4 (1999): 299. http://dx.doi.org/10.1071/mf98042.

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The subtropical rocky reefs of Cook Island, Julian Rocks and the South West Rocks area form part of a chain of islands and reefs with significant coral cover from the Queensland border (28˚S) to the southern extent of extensive coral communities in coastal Australia (31˚S). Benthic communities at 18 subtidal sites at the three localities were surveyed quantitatively by video-transects, and coral species lists were compiled. Twenty-eight coral species previously unrecorded for these localities were identified, increasing the species richness of hermatypic corals reported for the northern NSW re

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Grzelak, Katarzyna, and Piotr Kuklinski. "Benthic assemblages associated with rocks in a brackish environment of the southern Baltic Sea." Journal of the Marine Biological Association of the United Kingdom 90, no. 1 (2010): 115–24. http://dx.doi.org/10.1017/s0025315409991378.

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Sandy bottoms, with local patches of rocks, dominate the southern Baltic Sea coast. These rock patches create three-dimensional habitats with additional niches that can support diverse assemblages of organisms. In this study we investigated macrofaunal assemblages associated with the boulder field in the brackish Gulf of Gdansk. Of the 30 recorded taxa three animal species (Mytilus trossulus, Balanus improvisus and Electra crustulenta) together with five species of algae were directly attached to rocks. These engineering organisms provided habitats for a further 22 taxa. Among the fauna direct

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Gomes, Rickardo, and Valdeck Gomes. "The marble industry and its evolution since 1990 in Brazil: A bibliographic review." World Journal of Advanced Research and Reviews 19, no. 1 (2023): 062–68. https://doi.org/10.5281/zenodo.8437162.

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The Brazilian stoneworking industry has undergone various structural, cultural, and technological changes since the 1990s. The introduction of multi-wire saws has made extracting harder rocks such as quartzites possible, increasing productivity. The arrival of modern cutting and finishing machinery has facilitated the production of slabs and met the demands of an increasingly demanding and selective market. The use of resin treatments for slabs has been a significant advance. This context has elevated Brazil as one of the largest exporters of slabs for the external market while also becoming o

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SINCLAIR, BRADLEY J. "Two new synonyms from Tibet (Diptera: Empididae: Clinocerinae)." Zootaxa 4268, no. 2 (2017): 291. http://dx.doi.org/10.11646/zootaxa.4268.2.8.

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The subfamily Clinocerinae (Empididae, Diptera) are aquatic dance flies, most commonly encountered in fast flowing rocky streams and creeks. The adults often rest on emergent rocks and are rather common in temperate regions.

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Mack, Greg H., and T. Jerzykiewicz. "Provenance of post-Wapiabi sandstones and its implications for Campanian to Paleocene tectonic history of the southern Canadian Cordillera." Canadian Journal of Earth Sciences 26, no. 4 (1989): 665–76. http://dx.doi.org/10.1139/e89-057.

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Late Campanian to Early Paleocene sandstones of the Alberta Foothills were derived from three types of rocks: (i) andesitic–dacitic volcanic rocks that were presumably comagmatic with middle to late Mesozoic plutons in the Omineca Crystalline Belt; (ii) low-grade metamorphic rocks in the suprastructure of the Omineca Crystalline Belt; and (iii) sedimentary rocks in die Rocky Mountain Thrust Belt, principally pelitic rocks in the western Main Ranges and carbonates and chert-arenites in the eastern Main and Front ranges. A paucity of quartzo-feldspathic rocks fragments and potassium feldspar ind

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Peng, Yizhou, and I. Y. Grigorieva. "The reasons for the inheritance of the composition and properties of red-colored soils of the modern weathering crust within the western part of the Sichuan Basin of China." Geoèkologiâ, no. 3 (December 21, 2024): 44–58. https://doi.org/10.31857/s0869780924030057.

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In this work, we conducted an experimental evaluation and analysis of the characteristics and makeup of red-colored rocks from four representative Cretaceous and Jurassic sedimentary sequences in the western Sichuan Basin of China, as well as their weathering products. To determine the direction of weathering processes and the cause-and-effect link between the characteristics and composition of the parent rocks and the excess chemical components in the weathered soils, the chemical index of alteration was calculated. The findings demonstrated that, with regard to features like color, density o

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YATSENKO, Ivan, Sergey SKUBLOV, Ekaterina LEVASHOVA, Olga GALANKINA, and Sergey BEKESHA. "Composition of spherules and lower mantle minerals, isotopic and geochemical characteristics of zircon from volcaniclastic facies of the Mriya lamproite pipe." Journal of Mining Institute 242 (May 25, 2020): 150. http://dx.doi.org/10.31897/pmi.2020.2.150.

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The article presents the results of studying the rocks of the pyroclastic facies of the Mriya lamproite pipe, located on the Priazovsky block of the Ukrainian shield. In them the rock's mineral composition includes a complex of exotic mineral particles formed under extreme reduction mantle conditions: silicate spherules, particles of native metals and intermetallic alloys, oxygen-free minerals such as diamond, qusongite (WC), and osbornite (TiN). The aim of the research is to establish the genesis of volcaniclastic rocks and to develop ideas of the highly deoxidized mantle mineral association

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