Xenomorph (geology) - definition. What is Xenomorph (geology)
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%ما هو (من)٪ 1 - تعريف

CRYSTAL NOT BOUNDED BY ITS OWN CRYSTAL FACES
Allotriomorph; Allotriomorphic
  • Xenomorph of [[quartz]] crystals (grey) in [[granite]]

Xenomorph (geology)         
In geology, a xenomorph or allotriomorph is a mineral that did not develop its otherwise typical external crystal form because of late crystallization between earlier formed crystals. Xenomorphs are typical of matrix minerals in rapidly crystallizing volcanic lavas and shallow igneous intrusions.
Xenomorph (band)         
DUTCH DEATH METAL ROCK BAND
Xenomorph (Band)
Xenomorph is a Dutch death metal band formed in 1994 in Leiden, the Netherlands. The band is named after the Xenomorphs, fictional extraterrestrial creatures created by the Swiss artist H.
Diluvialist         
  • The [[Ark Encounter]], Kentucky, 2016 representation of Noah's ark, operated by [[Answers in Genesis]], a [[young Earth creationist]] organization.
  • pp=19–22}}
  • 2001}}
  • In the 18th century, finds such as [[Hutton's Unconformity]] showing layers tilted, eroded, and overlaid, demonstrated the "abyss of time" in the [[geologic time scale]].
  • Animals boarding Noah's ark, 1846 painting by [[Edward Hicks]].
  • angular unconformity]] found by [[James Hutton]] in 1788 at [[Siccar Point]] demonstrated the time taken for erosion of tilted rock and deposition of overlying layers.
ATTEMPT TO INTERPRET AND RECONCILE GEOLOGICAL FEATURES OF THE EARTH IN ACCORDANCE WITH A LITERAL BELIEF IN THE GLOBAL FLOOD DESCRIBED IN GENESIS
Vapor canopy; Creation geology; Canopy theory; Hydroplates; Hydroplate theory; Hydroplate; Vapour canopy; Canopy Theory; Creationist pseudogeology; Diluvial geology; Flood Geology; Catastrophic plate tectonics; Runaway subduction; Diluvialist; Diluvialism; Diluvial theory; Vailan theory
·noun One who explains geological phenomena by the Noachian deluge.

ويكيبيديا

Xenomorph (geology)

In geology, a xenomorph or allotriomorph is a mineral that did not develop its otherwise typical external crystal form because of late crystallization between earlier formed crystals. Xenomorphs are typical of matrix minerals in rapidly crystallizing volcanic lavas and shallow igneous intrusions. It is also typical of the interstitial or cementing minerals formed during the diagenesis of sedimentary rocks. The opposite is an idiomorph in which the external form is controlled only by the internal crystal structure.