Book contents
- Frontmatter
- Contents
- Preface
- Part I Principles
- Part II Siliciclastic sedimentary rocks
- Part III Carbonate sedimentary rocks
- Part IV Other chemical/biochemical sedimentary rocks and carbonaceous sedimentary rocks
- Chapter 12 Evaporites, cherts, iron-rich sedimentary rocks, and phosphorites
- Chapter 13 Carbonaceous sedimentary rocks
- References
- Index
- References
Chapter 12 - Evaporites, cherts, iron-rich sedimentary rocks, and phosphorites
from Part IV - Other chemical/biochemical sedimentary rocks and carbonaceous sedimentary rocks
Published online by Cambridge University Press: 05 June 2012
- Frontmatter
- Contents
- Preface
- Part I Principles
- Part II Siliciclastic sedimentary rocks
- Part III Carbonate sedimentary rocks
- Part IV Other chemical/biochemical sedimentary rocks and carbonaceous sedimentary rocks
- Chapter 12 Evaporites, cherts, iron-rich sedimentary rocks, and phosphorites
- Chapter 13 Carbonaceous sedimentary rocks
- References
- Index
- References
Summary
Introduction
This chapter deals with the chemical/biochemical rocks other than carbonates. Thus, it discusses evaporites, the siliceous sedimentary rocks (cherts), iron-rich sedimentary rocks (iron-formations and ironstones), and phosphorites. Volumetrically, these rocks are far less abundant than siliciclastic sedimentary rocks and carbonate rocks. If we add the percentages of shale, sandstone, and carbonate rocks calculated or measured by various authors such as Ronov et al. (1980), the unaccounted volume of total sedimentary rocks that can be attributed to these chemical/biochemical rocks appears to be no more than about 2 percent. The small volume of these rocks is not, however, a measure of their importance or the interest that we have in them. All of the sedimentary rocks discussed in this chapter have considerable economic significance. Evaporite deposits such as gypsum, halite (rock salt), and trona are mined for a variety of industrial and agricultural purposes, iron-rich sedimentary rocks are the source of most of our iron ores, phosphorites are extremely important sources of fertilizers and other chemicals, and the siliceous sedimentary rocks have some economic value, e.g. in the semiconductor industry.
In addition to their economic importance, all of the rocks discussed in this chapter are intrinsically interesting owing to their compositions and origins. The origin of many of these rocks is still enigmatic even after many years of study.
- Type
- Chapter
- Information
- Petrology of Sedimentary Rocks , pp. 461 - 526Publisher: Cambridge University PressPrint publication year: 2009
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