JPL Technical Report Server
The Formation of Chondrules: Petrologic Tests of the Shock Wave Model
Login
JPL TRS Home
→
JPL Technical Report Server
→
JPL TRS 1992+
→
View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
The Formation of Chondrules: Petrologic Tests of the Shock Wave Model
Connolly, H. C. Jr.
;
Love, S. G.
URI:
http://hdl.handle.net/2014/18995
Date:
1998-01
Citation:
Science
USA
Abstract:
Chondrules are mm-sized spheroidal igneous components of chondritic meteorites. They consist of olivine and orthopyroxene set in a glassy mesostasis with varying minor amounts of metals, sulfieds, oxides and carbon phases.
Show full item record
Items in TRS are protected by copyright, but are furnished with U.S. government purpose use rights.
Files in this item
Name:
98-0150.pdf
Size:
2.152Mb
Format:
PDF
View/
Open
This item appears in the following Collection(s)
JPL TRS 1992+
JPL TRS 1992+
Search
Search
This Collection
Browse
All Content
Communities & Collections
By Issue Date
Authors
Titles
Subjects
This Collection
By Issue Date
Authors
Titles
Subjects
My Account
Login
Register