(1) Cretaceous The most recent period of the Mesozoic era, 145 - 66 million years ago.

(2) Mesozoic Era complex plutonic masses from Shangyong area are composed of the plutones that are formed by Indosinian and Yanshanian cycle of structural magma and have different combination types.

(3) Mesozoic Era granites in northwestern Fujian can be generally classified into two types: remelting type and syntectic type.

(4) Ludong fault depression was a sub - depression of Kailu, which had a fold - fault basement of anti - Mesozoic era.

(5) The metallogenic ages are the lower and upper Proterozoic Subera, late and earlier Palaeozoic Era, Mesozoic Era, with Devonian Period as an important metallogenic era.

(6) Dulongjiang area is the north part of Burma-Malaya Geoblock of Gondwanaland. During th Mesozoic Era it collided with the Eurasian Plate, and became the southwestern borderland of East Asia Continent.

(7) Mammals arose from a fairly primitive reptile in the Mesozoic era.

(8) Anning Basin is a terringenous fault basin developed in Mesozoic Era.

(9) Many collisions of considerable size and periods of supervolcanism occurred early in the Mesozoic era.

(10) The exhalation-spout type deposits of the early Paleozoic era and the orogenic type deposits of the late Paleozoic to early Mesozoic era are the most important deposit groups.

(11) Songliao Basin is a expanding and rifted basin which was formed in Mesozoic era.