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Cretaceous:
third of the three periods included in the Mesozoic Era.  It began approximately 144 Ma and ended about 65 Ma.  It is noted for the deposition of the chalk of the white cliffs of Dover, England, and for the mass extinction of many invertebrate and vertebrate stocks.  Among these were the dinosaurs, mosasaurs, ichthyosaurs, plesiosaurs. 
extrusion tectonics:
two plates colliding and rising in elevation or an escape mechanism where part of one plate ???????
convergent margins:
a boundary between two lithospheric plates which are mloving towards each other.
dilational:
the process in which an applied stress leads to a state of strain involving a change in volume.  The change in volume is given by: <V = (Vf – Vo)/V03  where Vf  is the final volume and Vo is the initial volume.
fjord:
glaciated valleys now flooded by the sea
forearc prism sediments:
triangular section of deposits dragged in the subduction zone gap between two plates
glaciation:
the formation, advance and retreat of glaciers and the results of these activities.
gneiss:
a coarse, foliated metamorphic rock in which bands of granular minerals (commonly quartz and feldspars) alternate with bands of flaky or elongate minerals (e.g., micas, pyroxenes). Generally less than 50% of the minerals are aligned in a parallel orientation
gorge:
narrow steeply sided canyon typically eroded by water along a fault line
island arc:
a curved chain of islands that develops between an oceanic trench and a continental landmass.
isotopic dating:
a means of determining the age of certain materials by reference to the relative abundance of the parent isotope (which is radioactive) and the daughter isotope (which may or may not be radioactive).  If the decay constant (the half-life or disintegration rate of the parent isotope) and the concentration of the daughter isotope are known, it is possible to calculate an age. 
MA:
million years ago
magnetite:

iron oxide; Mineral, Fe3O4; Color: black; SG: 5.2; Hardness: 5.5 - 6.5; Comments: ore of iron, strongly magnetic

mantle:
that portion of the Earth below the crust and reaching to about 2,780 km, where a transition zone of about 100 km thickness separates it from the core. It has a high iron, magnesium and nickel composition.
metamorphism:
the process of changing the characteristics of a rock in response to changes in temperature, pressure, or volatile content.
oceanic plate:
lithospheric plate made primarily of dense maphic material
orogeny:
the process of mountain building due to tectonic activity at  or aligned with convergent plate margins.
pH:
the negative logarithm of the hydrogen ion concentration. It is commonly used as a measure of acidity. It has a range from 1 to 14. The lower the number the more acidic the solution.
rifting:
a breach or split between two bodies due to rising hot spot activity within the mantle. Continuous activity thins the lithospheric plate, causes normal and reverse dip-slip faulting and eventually separates the plate.
sedimentary rock:
rock formed by the deposition and compression of mineral and rock particles, but often including material of organic origin.
strike slip fault:
a fault in which the major displacement is horizontal and parallel to the strike of a vertical or subvertical fault plane. Movement along such a fault may be dextral or sinistral.
subduction zone:
a narrow, elongate region in which one lithospheric plate is forced under another by tectonic activity.
supercontinent:

a continental mass that includes several of the cratons of the present-day continents. The last supercontinent (Pangea) broke apart approximately 250 Ma.

tailings:
fine waste material from a mineral-processing plant, that is too poor for further treatment.
tectonic:
deformation within the Earth’s crust, and its consequent structural effects due to active plate movement.
trench
a long, narrow, steep-walled, often arcuate depression in the ocean floor, much deeper than the adjacent ocean and associated with a subduction zone