Institution
Rio de Janeiro State University
Education•Rio de Janeiro, Brazil•
About: Rio de Janeiro State University is a education organization based out in Rio de Janeiro, Brazil. It is known for research contribution in the topics: Population & Large Hadron Collider. The organization has 16631 authors who have published 30919 publications receiving 465753 citations. The organization is also known as: UERJ & Rio de Janeiro State University.
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TL;DR: In this article, aqueous dispersions based on 4,4′-dicyclohexylmethane diisocyanate (H12MDI), poly(propylene glycol) (PPG) and dimethylolpropionic acid (DMPA) were synthesized.
174 citations
TL;DR: The overall GRADE analysis was very low for migraine and seizures, low for superficial venous thrombosis,Thrombocytopenia, chorea, longitudinal myelitis and the so-called seronegative APS and moderate for APS nephropathy, heart valve lesions and livedo reticularis.
173 citations
TL;DR: Present analysis indicated that SAD cannot be interpreted as atypical forms of SCH or MD and does not appear to represent a SCH and MD comorbidity or yet an independent mental disorder.
172 citations
TL;DR: The Araçuaí orogenic orogen extends from the eastern edge of the São Francisco craton to the Atlantic margin, in southeastern Brazil as mentioned in this paper, forming the Eastern Brazilian pegmatite Province and the most important dimension stone province of Brazil.
Abstract: Abstract The Araçuaí orogen extends from the eastern edge of the São Francisco craton to the Atlantic margin, in southeastern Brazil. Orogenic igneous rocks, formed from c. 630 to c. 480 Ma, cover one third of this huge area, building up the Eastern Brazilian Pegmatite Province and the most important dimension stone province of Brazil. G1 supersuite (630–585 Ma) mainly consists of tonalite to granodiorite, with mafic to dioritic facies and enclaves, representing a continental calc-alkaline magmatic arc. G2 supersuite mostly includes S-type granites formed during the syn-collisional stage (585–560 Ma), from relatively shallow two-mica granites and related gem-rich pegmatites to deep garnet-biotite granites that are the site of yellow dimension stone deposits. The typical G3 rocks (545–525 Ma) are non-foliated garnet-cordierite leucogranites, making up autochthonous patches and veins. At the post-collisional stage (530–480 Ma), G4 and G5 supersuites were generated. The S-type G4 supersuite mostly consists of garnet-bearing two-mica leucogranites that are the source of many pegmatites mined for tourmalines and many other gems, lithium (spodumene) ore and industrial feldspar. G5 supersuite, consisting of high-K–Fe calc-alkaline to alkaline granitic and/or charnockitic to dioritic/noritic intrusions, is the source of aquamarine-topaz-rich pegmatites but mainly of a large dimension stone production.
172 citations
TL;DR: This initial study provides the framework for more focused studies of this subject, which are necessary to determine whether the changing balance of NK receptor expression may influence susceptibility to infectious, inflammatory, and neoplastic diseases.
171 citations
Authors
Showing all 16818 results
| Name | H-index | Papers | Citations |
|---|---|---|---|
| Hyun-Chul Kim | 176 | 4076 | 183227 |
| Maria Elena Pol | 139 | 1414 | 99240 |
| Wagner Carvalho | 135 | 1395 | 94184 |
| Alberto Santoro | 135 | 1576 | 100629 |
| Andre Sznajder | 134 | 1464 | 98242 |
| Luiz Mundim | 133 | 1413 | 89792 |
| Helio Nogima | 132 | 1274 | 84368 |
| D. De Jesus Damiao | 128 | 1162 | 82707 |
| Magdalena Malek | 128 | 598 | 67486 |
| Sudha Ahuja | 127 | 1016 | 75739 |
| Helena Malbouisson | 125 | 1151 | 82692 |
| Jose Chinellato | 123 | 1116 | 64267 |
| Flavia De Almeida Dias | 120 | 590 | 59083 |
| Gilvan Alves | 119 | 829 | 69382 |
| C. De Oliveira Martins | 119 | 880 | 66744 |