DOC PREVIEW
UA GEO 102 - basic principles of rocks
Type Lecture Note
Pages 3

This preview shows page 1 out of 3 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 3 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 3 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

GEO 102 Lecture 12Outline of Last Lecture I. Geologic TimeOutline of Current Lecture II. Types of unconformitiesIII.CorrelationIV.Absolute DatingV.Half-lifeCurrent LectureBasic Principles of Rock Formation-Cross-cutting relationships: If one rock formation intrudes or bisects another, the rock being cross-cut must be older-Also inclusionsBasic Principles of Rock Formation-Unconformities-Non-deposition-ErosionAs opposed to a conformable transitionTypes of Unconformities-Angular unconformity-Rocks were tiled prior to later sedimentation-disconformity-Erosional surface between 2 parallel layers of rock-nonconformityThese notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.-Sedimentary rocks in contact with non-sedimentary rocks Most of these are based on simple fundamental logic – it almost seems unnecessary to define them.-The Really Big Picture-How do we take the previous interpretation of a single outcrop and extrapolate global time?-Correlation-Linking outcrops of the same rock over wide areas-Even globallyCorrelation-Linking time-equal rocks-Presently many different depositional environments form simultaneously.-Later they will be preserved incompletely as a wide range of rocksHow do you link the outcrops?-Rock types-Geochemistry-Fossils-Fossil succession-Fossils change in an orderly way through time-Index fossils-Extinction and evolution-Absolute datingAbsolute dating-Relative dating has been around centuries, and, but absolute estimates of the age of theEarth varied.-The goal was a fixed and absolute age-Radioactivity can act as a clock Decay and Half-life-Unstable nuclei eject particles predictably in order to achieve equilibrium-alpha particles ()-2 protons and 2 neutrons-beta particles ()-Electron from nucleus-Electron capture-Forms a neutron after fusing with a protonHalf-Life-For any given atom, it can not be predicted when decay will occur-However, a POPULATION of atoms will decay like clockwork-the time it takes for half of the population to decay = one half-lifeWhat do we date?-Only some elements have radioactive isotopes-Only some isotopes have half-lives that are useful-Only some minerals contain these few isotopes-Only some rocks contain pristine minerals-There must be no non-radioactive alteration of parent or daughter-Closed


View Full Document

UA GEO 102 - basic principles of rocks

Type: Lecture Note
Pages: 3
Download basic principles of rocks
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view basic principles of rocks and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view basic principles of rocks 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?