a) Large plagioclase laths entrapped in fine groundmass. (b)... | Download Scientific Diagram
%204.1g%20(700).jpg "Unusual Meteorite Features (NWA 3147 with Plagioclase Laths visible in crust) - Meteorites Australia")
Unusual Meteorite Features (NWA 3147 with Plagioclase Laths visible in crust) - Meteorites Australia
Basalt, showing typical diabasic structure of lath-shaped crystals of plagioclase, vintage line drawing or engraving illustration Stock Vector Image & Art - Alamy
Proc. IODP, 330, Site U1374
A) Basalts with stretched and aligned plagioclase laths B) basalt... | Download Scientific Diagram
Photomicrograph showing (a) Oscillatory zoning of plagioclase (XPL),... | Download Scientific Diagram
Andesite intrusions of the Chicxulub structure
Photomicrograph showing undeformed plagioclase laths and amygdales in... | Download Scientific Diagram
Bulletin of the British Museum (Natural History), Mineralogy. VOLCANIC ROCKS FROM THE CAPE VERDE ISLANDS 57 The rock is dark grey, highly vesicular, with scattered phenocrysts of plagioclase, pale titanaugite, and
plagioclase | Life in Plane Light
Figure F11. Typical mineralogy and textures of upper series lavas. A. Bow-tie intergrowth of plagioclase and clinopyroxene of a moderately plagioclase-olivine-clinopyroxene phyric basalt (Unit I-1; Sample 163X-SEG57A-1-1, 18–22 cm). The groundmass is
04944590015476714301527.jpg
Plagioclase laths tangentially arranged around olivine in a picrite... | Download Scientific Diagram
a Growth of new sillimanite laths with tiny plagioclase inclusions and... | Download Scientific Diagram
Figure F16. Olivine phenocrysts partially altered to brown smectite but with unaltered interiors in Sample 192-1187A-6R-6 (Piece 2C, 105-107 cm). The groundmass consists of radiating elongate plagioclase laths and small interstitial crystals
Thin sections micrographs of the studied andesites: a) plagioclase... | Download Scientific Diagram
.jpg "ALEX STREKEISEN-Ophitic-")
ALEX STREKEISEN-Ophitic-
Olivine Basalt
![Figure F35. Pillow margin showing plagioclase laths defining a subtrachytic texture around an altered olivine phenocryst (highlighted) (Sample 192-1186A-31R-1 [Piece 3B, 44-48 cm]) (field of view = 5.5 mm; crossed polars; photomicrograph](http://www-odp.tamu.edu/publications/192_IR/chap_06/images/06_f35.jpg "Figure F35. Pillow margin showing plagioclase laths defining a subtrachytic texture around an altered olivine phenocryst (highlighted) (Sample 192-1186A-31R-1 [Piece 3B, 44-48 cm]) (field of view = 5.5 mm; crossed polars; photomicrograph")
Figure F35. Pillow margin showing plagioclase laths defining a subtrachytic texture around an altered olivine phenocryst (highlighted) (Sample 192-1186A-31R-1 [Piece 3B, 44-48 cm]) (field of view = 5.5 mm; crossed polars; photomicrograph
Plagioclase thin section - Tectosilicates - MicROCKScopic
![Figure F31. Unaltered interiors of olivine phenocrysts (small equant crystals [center]) at the center of a variole defined by radiating, skeletal plagioclase laths in Sample 192-1185A-11R-1 (Piece 4B, 83-86 cm), Unit 5B (](http://www-odp.tamu.edu/publications/192_IR/chap_05/images/05_f31.jpg "Figure F31. Unaltered interiors of olivine phenocrysts (small equant crystals [center]) at the center of a variole defined by radiating, skeletal plagioclase laths in Sample 192-1185A-11R-1 (Piece 4B, 83-86 cm), Unit 5B (")
Figure F31. Unaltered interiors of olivine phenocrysts (small equant crystals [center]) at the center of a variole defined by radiating, skeletal plagioclase laths in Sample 192-1185A-11R-1 (Piece 4B, 83-86 cm), Unit 5B (
Annual report . with crossed nicols. The phenocrysts are set in agroundmass which is made up dominantly of irregular plagioclase laths showing albitetwinning lamellae, giving a maximum extinction angle of 20
Acklington Dyke - Geology North
The formation of plagioclase chains during convective transfer in basaltic magma | Nature
a) Photomicrograph of aligned plagioclase laths (pl) and elongate... | Download Scientific Diagram
Phenocryst - Wikipedia
