magma造句121. This rock type originates in the magma chambers that underlie volcanoes.
122. Beneath the sediment, along the accretionary front, the sinking Arabian plate heats up under extreme pressure and rock melts into magma.
123. The addition of the crustal materials into the magma played an important role in promoting the liquation processes.
124. The magma mingling between mafic magma and felsic magma is the primary mechanism responsible for the granitoids of crust-mantle mixed source.
125. Some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.
126. The metallogenic material was from deep alkalic basaltic magma , and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
127. The Jurassic volcanic rocks are belong to K alkaline and came from shallow crust with weak repartition of magma.
128. The magma falls as volcanic bombs which accumulate around the vent and form steep-sided cones.
129. The intrusion of magma affected the orogenesis and deformation and it is an important geological process and factor leading nonlinear deformation.
130. Eruptions begin with an upwelling of magma from earths hot interior.
131. Augite monzonite crystallized at high-temperature and over-hypabyssal conditions. The water-deficient, highly viscous magma was favourable to the formation of the volcanic dome.
132. Besides,[www.] we also find that there are magma thermal actions during the Carboniferous period and early Permian period.
133. Granitoid composition is controlled by tectonic settings, magma sources, initiation and evolution processes.
134. The enclaves are remnants of rocks which partially melted to form granitoid magma.
135. Abstract: The Lower Paleozoic carbonates of Tarim Basin were marbleized locally due to the thermal effects of magma intrusions.
136. In many places surface rocks have been melted, baked by the heat of magma beneath.
137. I am a volcano quiet in many years, i wish one day the magma burry in my mind will spout to the sky!