"Diamonds, Meteorites and the Origin of the Solar System", 2006-11-07, De Carli

The pre-lecture dinner (5:30 pm in GeoCorner Room 320-109) requires reservation no later than 11/03/06, and is $30 regular, $5 for students; however no-shows owe full price.

Abstract

The title of this talk is also the title of a paper by Nobel Laureate

Harold Urey, published in the Astrophysical Journal 50 years ago. Most

meteorites last solidified from melt about 4.5 billion years ago, making

them the oldest objects available for study. The major motivation for the

study of meteorites is to use the evidence in meteorites to test models of

the early history of the solar system. For Urey, the fact that diamonds

were found in some meteorites implied that these meteorites must have once

been deep within a larger body, at least as big as the moon, at pressures

within the stability field of diamond. His model was undone by SRI

experiments showing that diamonds could be made by shock wave compression

and by the one-to-one correlation between presence of diamond and

metallurgical evidence for high shock pressures in individual meteorite

fragments.

The study of meteorites is truly interdisciplinary: Geochemists analyze and

date individual mineral grains, Metallurgists study diffusion profiles and

shock wave metamorphic effects to interpret thermal histories of

iron-nickel meteorites, Mineralogists and Shock Wave Physicists team to

interpret the shock pressure-temperature histories of deformational

features of stony meteorites.

This talk will give a broad overwiew of the current state of meteorite

research, with emphasis on the speaker's interests in shock wave effects

such as formation of high-pressure phases. Effects of large impacts,

including dinosaur extinction, the "big whack" model for formation of the

Moon, and delivery of Martian meteorites to the Earth, will be briefly

touched upon.

About the Speaker

http://www.diggles.com/pgs/2006/Paul06.jpg (photo of Paul)

Paul S De Carli is a Senior Scientist Emeritus at SRI International and an

Honorary Research Fellow in Earth Sciences at the University College

London. He writes: "I was drafted to give a talk at the Sept. meeting of

the American Society for Materials. After going to the work of preparing

that talk, I'd be happy to give it again to the PGS. I'd modify the talk

slightly, with more emphasis on high-pressure mineralogy and less emphasis

on metallurgy. One of our PGS regulars, Bob Wallace, was at the ASM meeting

and thought the talk would be appropriate for the PGS."

There is another page or two of interesting information about Paul's long

career at http://www.diggles.com/pgs/2006/PGS06-11.html

 
Date and Time:
 Tuesday, November 7, 2006.  7:30 PM.
Approximate duration of 1.5 hour(s).
Location:
GeoCorner Room 320-105  [Map]
URL:
Audience:
General Public
Category:
Meetings
Sponsor:
Peninsula Geological Society
Contact:
(650) 736-2215
cgm@pangea.stanford.edu
Admission:
The lecture is free.
Download:
Print:
Last Modified:
November 2, 2006