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The results (Table 1) revealed that the pink centered white fluidal colonies were devoloped on Triphenyl tetrazolium chloride agar and SMSA media; cream or off-white colored colonies on Casamino peptone glucose agar, Yeast extract agar and Potato dextrose agar; creamy white and dull white colonies on Nutrient agar, Yeast extract peptone agar and Yeast extract milk agar and yellow colored colonies on Yeast extract chalk agar were developed of the bacterium R.
The fluidal vesicular lava interlayers are dominant with respect to the clastogenic massive lava inter-layers, which are more common at the upper part of the East Quarry section.
Los microlitos de plagioclasa (55%) son de habito tabular y disposicion fluidal, y por su morfologia, esqueleticos.
Bacterial colonies developing the typical fluidal, irregular and creamy white with pink at the centre, colony was selected and subjected to colony polymerase chain reaction (PCR) using R.
Fluidal colonies with reddish pink center and irregular margins are usually virulent while dark colored non-fluidal colonies with darker colors and smooth margins are normally avirulent.
Las rocas de composicion riodacitica son de color gris claro, amarillento o rosado, de grano mediano, porfidicas y con matriz mas o menos fluidal.
La matriz es microlitica fluidal y los minerales que componen la roca son oxihornblenda, biotita, plagioclasa y ortopiroxenos.
En seccion delgada, la matriz puede alcanzar hasta un 60-75%, es microcristalina o criptocristalina con o sin vidrio, con microlitos de plagioclasa definiendo una textura fluidal --raquitica FIGURA 2, y los fenocristales pueden alcanzar hasta un 50-55%.
Igneous zircons in a rhyodacitic dome with fluidal texture, intruded in ignimbrites of the lower part of this formation, were dated at 327,9 [+ or -] 2.
diabasico del cerro Las Bolas (6,4-6,2 Ma) y en un dique andesitico rico en plagioclasa con marcada estructura fluidal (6,1 Ma), presente en la quebrada La Danta (MacMillan et al.
12, medium-grained structure, and intergranular and rare fluidal texture, marked by the arrangement of platy minerals (plagioclases), were observed.
In that location the ignimbrite does not have a defined base, with a vitrophyre, but rather appears to continue downward into fluidal rhyolites, suggesting that the ignimbrite corresponds to an intracaldera facies rather than an outflow sheet.