NAME: OMOSANYA OLUBUNMI ESTHER
MATRIC NO: LCU/UG/23/26508
COURSE TITLE: ENGINEERING GEOLOGY (PRATICAL 10)
COURSE CODE: CVE 301
SUBMITERD TO:
DEPARTMENT OF CIVIL ENGINEERING
THE FACULTY OF ENGINEERING
LEAD CITY UNIVERSITY, IBADAN, NIGERIA
LECTURER-IN-CHARGE:
ENGR. FASASI & ENGR ITUNU
Figure 1: Map showing the Nigerian basement complex terrain. (Obaje, 2009)
(iv) Older granites, which comprise rocks varying in composition from granodiorites to true
granite and potassic sysnite.
(v) The unmetamorphosed dolerite dyke is believed to be the youngest.
These rocks are believed to have been emplaced during the Pan-African Orogeny and are
therefore thought to be of Pan-African age (i.e 600 ±150m.years (Ramahan, 1988, Odeyemi,
1982.
SEDIMENTARY BASIN
Sedimentary basins are large depressions where sediments accumulate over millions of
years, often forming important reservoirs of natural resources such as petroleum, natural gas, and
4. Granites: Coarse-grained igneous rocks that intrude the Precambrian Basement Complex.'
Fi
gure 2: Geological map of oyo