... (sUAS, also known as drones) with onboard cameras can supplement those data at a relatively low cost. The advantage of using sUAS and other remote surveying systems is twofold: (1) they can cover a relatively large area in a short time; and (2) they can take images of regions that may be difficult...

... states. It unconformably overlies the Sanga do Cabral Formation in the Rio Grande do Sul state and the Pirambóia Formation in the Paraná state and is unconformably overlain by the Botucatu Formation in both states ( Scherer et al., 2023 ). In Uruguay, the Batovi Member of the Tacuarembó Formation, which...

... Jurassic (J 2 )), and pre-Jurassic (crust of weathering (CW) of the Paleozoic) deposits of the Shaim (ShS) and Verkhnepurskii (VS) swells; the Verkhnekondinskii (VD), Sherkalinskii (ShD), and Yarsomovskii (YaD) deflections; the Krasnoleninskii (KA), Surgut (SUA), Nizhnevartovskii (NA), and Northern (NOA...

... 4.0–38.6 mm (average = 20.2 mm, N = 7). Sterile ultimate appendages (SUAs).—In only two specimens, ultimate appendages that are probably sterile are found attached to the base of first-order branches, but they are very poorly preserved, with only a short, undivided fragment left ( Fig. 6.6 – 6.10...

... (review) 94 I1 terremoto del 24 Gennaio, 1912 , nelle Isole Jonie e sua veloeita di propagazione (review) . . . . . . . . . . . . . . . . . . . . . 94 Allen, C. GReviews of three papers by Agamennone . . . . . . . . 93, 94 BalIore, Montessus de--The so-called luminous phenomena of earthquakes...

... & Danni 1979 , Teixeira et al. 1987 , Brenner et al. 1990 ). Serpentine–tremolite –talc–chlorite-bearing rocks constitute the most abundant member of this sequence, with intercalation of banded iron-formation (oxide and silicate facies), graphite–pyrrhotite–pyrite-bearing metacherts and basaltic...

... of the original diagnosis from Frest and Strimple ( 1981 ), which had been removed in the emended diagnosis of Eckert and Brett ( 2001 ). However, the main change in the diagnosis is that the members of the family may have 10 or 20 biserial arms, as in Tormosocrinus and Meperocrinus n. gen., the only two...

... of Travagini’s book was in fact Henri-Louis Habert de Montmor (1600–1679), a French scholar and scientist, elected to the Académie française in 1634, and member of Louis XIV King’s council ( Figure 4 ). Montmor gathered learned friends (including Gassendi, Desargues, Rohault, Roberval, Huygens, and others...

... developed his knowledge and abilities to become a botanist—a ‘call’ he could not resist. Amongst other networks, he was a member of the Württemberg Botanical Travel Association, Unio Itineraria. Belonging to scientific societies, especially those devoted to natural history, was quite a relevant activity...

..., PetroMod™ is used to model the basin. Figure 1. A GBM workflow, illustrating how the basin model via rock-physics operations can be used in tomography and seismic uncertainty analysis (SUA). 30 12 2014 6 5 2015 11 5 2015 2015 Society of Exploration Geophysicists...

.... Table 4 shows that several of the samples also contain calcite. Representative electron microprobe analyses of the carbonates in the samples from the Águas Claras deposit are given in Table 5 . All turn out to be relatively close to the dolomite end member, except for some ferroan dolomite in sample...

.... For these reasons, this basin is considered as the type basin for these cycles, and tentative correlation and synchronization with other basins are made in this report ( Fig. 7 ). The cycle corresponds to the “Paripueira Evaporite Beds,” located in the lower part of the Maceió Member of the Muribeca...

... of the calcareous clasts decreases from 30 cm in average to 2 cm in average going from NE to SW (present day coordinates); the calcarenitic to micritic matrix increases upwards. At Timpa di Mezzogiorno (North of the Orsomarso village), four samples have been collected in the Alberosa Member (MDE13-MDE16...

... the beginning of a survey through a series of interviews with members of the guild of Venetian fishermen of San Nicolò (the so-called ‘ Nicolotti ’) witnesses to the changes in the waters and the seabed where they labored. Figure 8. A manuscript copy of Castelli’s Considerazione intorno alla Laguna di...

.... & Di Celma C. 2011 . Taphonomic and paleoecological analyses (mollusks and fishes) of the Súa Member condensed shellbed, Upper Onzole Formation (Early Pliocene, Ecuador) . Palaios 26 , 160 –72. Chapman...

... important scientist, Robert Boyle (1627–1691), a member of the Royal Society of London, who performed several experiments on magnetism, and concluded that a brick could acquire a magnetization upon cooling from high temperatures and could then become capable of attracting a compass needle ( Boyle 1691...

... ( Table 1 ). All of the fossil decapods previously reported from localities in Istria are brachyurans, and the overwhelming majority of the occurrences are of species of Harpactocarcinus A. Milne Edwards, 1862 and Harpactoxanthopsis Via, 1959 , both members of the extinct family Zanthopsidae Via...

.... Equation 3 is the fitted function. (3) X T = a 3 ⋅ Sa − a 4 ⋅ Ca where: Sa is the BET–SSA (m 2 /g); Ca is the CEC (μEq g/g); a 3 = (3.0±0.3) μmol/m 2 and a 4 = (1.2±0.2) μmol/μEqg are empirical constants. When both members in equation 3 are divided by Sa, equation 4...

... discussed. 17 01 2011 2011 PODOCNEMIDOID TURTLES are formed, according to Gaffney et al., (2006) , by the two most diverse groups of pleurodires or side-necked turtles: the extinct Bothremydidae and the extant and fossil members of Podocnemididae plus Brasilemys josai Lapparent de...

... , rather than species of Channa , and is here described as a new species, Parachanna fayumensis . It differs from the other species of the genus in possessing a prominent tooth patch on the posterior end of the parasphenoid. This new species of channid is the oldest member of the family known from Africa...