Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
| Authors: |
|
|
|---|---|---|
| Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
| Type: | Resource | |
| Storage: | The size of this resource is 3.7 MB | |
| Created: | Mar 23, 2020 at 5:21 p.m. | |
| Last updated: | Mar 30, 2020 at 6:52 p.m. | |
| DOI: | 10.4211/hs.37022ed885554039b024a0f1c740a3e0 | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
|---|---|
| Views: | 1001 |
| Downloads: | 44 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
These data are the results for the 2020 GEOL 5321 NMR lab. Measurements were made on the Corona NMR with sieved play sand. The grains consist of: majority quartz, lesser feldspar, trace mica and lithic fragments.
Subject Keywords
Content
Related Resources
| This resource has been replaced by a newer version | Elliot, M. (2020). Lab nuclear magnetic resonance (NMR): controls of variable grain size on relaxation response, HydroShare, http://www.hydroshare.org/resource/f67f56c185ff4369a303e9a9176d92bb |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| NSF | 1829100 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
|---|---|---|---|---|
| Dr. Andy Parsekian | University of Wyoming |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment