Sec 070 room 201 prerequisite geol 3056
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University of Puerto Rico Mayagüez Campus Department of Geology Sedimentary Environments and Lithogenesis GEOL-4046 Dr. Hernán SantosOffice: F-412, ext. 3583 Office Hours: Monday and Wednesday 8:35-11:35 AM. Sec-070 Room 201 Prerequisite: Geol 3056.

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Sec-070 Room 201 Prerequisite: Geol 3056

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Sec 070 room 201 prerequisite geol 3056

University of Puerto RicoMayagüez CampusDepartment of GeologySedimentary Environments and Lithogenesis GEOL-4046Dr. Hernán SantosOffice: F-412, ext. 3583Office Hours: Monday and Wednesday8:35-11:35 AM

Sec-070 Room 201

Prerequisite: Geol 3056


University of puerto rico mayag ez campus department of geology sedimentary environments and lithogenesis geol 4046

Objective of course:This courses provide the students with the knowledge to identify sedimentary rocks, sedimentary structures, to understand the processes of erosion, transportation, and deposition, and to associate the rocks to environments of deposition.


Description of the course

Description of the course:

  • Introduction to the processes of sedimentary rock formation, including the weathering of rocks, and the transportation, deposition, and lithification of sediments.

  • Emphasis on the field study of diverse modern sedimentary environments and classification of sedimentary rocks based on petrographic analysis.


University of puerto rico mayag ez campus department of geology sedimentary environments and lithogenesis geol 4046

Sedimentary Environments and Lithogenesis($99.35, University Bookstore)Text Book: Sedimentary Geology, 2nd Ed.Author: Donald R. Prothero and Fred SchwabEdit. House: Freeman1st ExamSeptember 28Sedimentary Rocks: An IntroductionChapter 2- WeatheringChapter 3- Clastic Transport and Fluid FlowChapter 5- Sandstones and ConglomeratesChapter 6- Mudrocks2nd ExamNovember 2Chapter 8- Terrestial Sedentary EnvironmentsChapter 9- Coastal EnvironmentsChapter 10- Silisiclastic Marine and Pelagic Env.3rd ExamDay of Final ExamChapter 11-Carbonates RocksChapter 12- Carbonate EnvironmentsChapter 13-Other Biogenic Sedimentary RocksChapter 14-Chemical and Non-Epiclastic Sedimentary Rocks


Grading

Grading:

  • The final grade of the class will consist of 60% class grade:

    • 3 partial exams

    • A Final Report

    • A total of 400 points

  • 40% laboratory grade.


Final report

Topics: (examples)

Microbial build-ups

Deltas

Eolian systems

Eruption processes and facies

Glaciers and glaciers deposits

Volcanic eruption processes and facies

Deep water processes and products

Shallow water carbonates

Lacustrine processes and deposits

Reef structures and sediments

Sept 15 Topic of report and 3 references

7 to 15 pages including figures and 3 references

3-7 references

Should include:

title page

Index

Introduction

body

references

numbered pages

Final Report


Sedimentary rocks an introduction

Sedimentary Rocks: an Introduction

  • Sedimentology- the study of the processes that erode, transport, and deposit sediments.

  • Sedimentary petrology- the characteristics and origins of sedimentary rocks.


Analysis of sedimentary rocks involves description and interpretation

Analysis of sedimentary rocks involves“description” and “interpretation”

  • We will learn to describe sedimentary rocks

  • Look for characteristics that will help us to determine the environment of deposition.


Conglomerate

Conglomerate

  • Composed of pebbles of preexisting rocks and minerals. Clasts-broken fragments.

  • Color.

  • Composition of clasts of rocks and minerals.

  • Texture- refers to the size, shape, arrangement of the grains the make up the rock.

    • Roundness


Texture

Texture

  • Clastic- composed of individual fragments that were transported and deposited as particles.

  • Crystalline- results from the in situ precipitation of solid mineral crystals.


Texture refers to the size shape arrangement of the grains the make up the rock

Texture- refers to the size, shape, arrangement of the grains the make up the rock.

  • Grain size- grain diameter (boulders, pebbles, cobbles, sand, silt, or clay).

  • Shape- is described in terms of sphericity

  • Roundness or (angularity) refers to the sharpness or smoothness of their corners.


Sedimentary structures

Sedimentary Structures

  • Large scale, three-dimensional features of sedimentary rocks best studied in outcrops

  • The most important is stratification- the banding or layering exhibited by as consequences of deposition of the clasts grain by grain over time.

  • Ripple marks, raindrop imprints, mud cracks, cross-bedding, ripple marks.


Fossil content

Fossil content

  • Sedimentary rocks often contains organic remains, either hard parts (shells, bones, or their replacement) or trace of organism such as tracks, trails, burrows (ichnofossils).


Sedimentary rock interpretation a case study

Sedimentary rock Interpretation: A case study

  • What do we really want to know about any sedimentary rock?

  • What information can be inferred from each of the physical characteristics?

  • We seek the answer to rather simple questions.


We seek the answer to rather simple questions

We seek the answer to rather simple questions.

  • 1. When was the sedimentary rock unit deposited, and over how broad a region?

  • 2. With what other rock units is the sedimentary rock contemporaneous?

  • 3. From what kinds of source rocks were the sediments derived?

  • 4. Where was that source located? Was it near or far from the depositional site, and in what direction?


University of puerto rico mayag ez campus department of geology sedimentary environments and lithogenesis geol 4046

  • 5. Was the source a mountainous highland or an area of low relief?

  • 6. How was the material transported to the depositional site from the area where it was weathered and eroded? Was it blown by the wind, bounced along the channel of flowing river, moved by the surf and longshore currents, or carried by a sheet of slow-moving glacial-ice?

  • 7. In what kind of physical setting did the sedimentary rock form? Was it deposited by an ancient river delta system? Is it a lithified desert dune complex?


University of puerto rico mayag ez campus department of geology sedimentary environments and lithogenesis geol 4046

  • 8. How have the color, composition, texture, and other physical properties of the sedimentary rock been modified in the time since deposition?

  • Answering these questions helps us understand the genesis of a sedimentary rock. Answers to such questions are formally embodied as stratigraphy, provenance, dispersal, transporting agent, depositional setting, paleo-geography, sedimentary tectonics, and diagenesis.


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