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C 第一章 岩石和构造2-岩浆岩
昆明理工大学土木系 徐则民
2005/09/29
工程地质学
第三讲
1.2 岩石
根据成因,构成地壳的岩石可以分为岩浆岩、沉
积岩和变质岩三大类。
岩石循环
活动断裂(地震)主要分布板块边界上,有时也
受板块内部的超壳断裂控制的控制
全球板块构造略图
Cliff Erosion
Devils Tower Wyoming
The exposed rocks at Devils Tower National
Monument are classified into two general
types: igneous and sedimentary. The tower
itself is composed of igneous rock formed by
cooling and crystallization of once-molten
materials. The rocks exposed around the tower
are sedimentary-layers of shale, sandstone, silt
stone, mud stone, gypsum, and limestone.
They were formed by the consolidation of
fragmented materials derived from other rocks
or the accumulation of chemical precipitates
that were deposited on the floors or near the
shores of ancient seas. Devils Tower owes its
impressive height to the differing rates of
erosion of these two rock types-the soft
sedimentary rocks have eroded more readily
than the hard igneous rock. One of the most
striking features of the tower is its polygonal
columns, formed as the igneous mass slowly
cooled and crystallized. Most of the columns
are 5-sided, but some are 4-sided or 6-sided.
Numerous cross-fractures in the upper part of
the tower divide the columns into many small,
irregularly-shaped blocks. [Photo credit:
Michelle Flores, National Geophysical Data
Center.]
颜色及成分变化构成的水平层理
西藏昌都, 2001/7/4
具有斜层理的第四系半胶结砾岩 金沙江水富段
Arizona has some of the most spectacular geology anywhere! The Grand Canyon, the worlds premier
geologic locality, exposes 1.7 billion years of geologic history in its walls. The photograph to the left
shows a beautiful view of the Grand Canyon, with its upper flat-lying layers of Paleozoic limestone,
sandstone, and mudstone.
From:/research/az_geology/az_geology.h
tml
Intensely foliated micaceous phyllites of the Malmesbury Group, Cogmans
Kloof Pass
千枚
岩
http://
www.
uct.ac.
za/de
pts/ge
olsci/d
lr/4da
y2001
/index.
html#
4day
Phyllites of the Malmesbury Group forming the basement to the Table
Mountain Group, Cogmans Kloof Pass
h
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