- Home
- Science
- Earth Sciences
- Fluid-Fluid Interactions
Fluid-Fluid Interactions
List Price:
$51.99
- Availability: Confirm prior to ordering
- Branding: minimum 50 pieces (add’l costs below)
- Check Freight Rates (branded products only)
Branding Options (v), Availability & Lead Times
- 1-Color Imprint: $2.00 ea.
- Promo-Page Insert: $2.50 ea. (full-color printed, single-sided page)
- Belly-Band Wrap: $2.50 ea. (full-color printed)
- Set-Up Charge: $45 per decoration
- Availability: Product availability changes daily, so please confirm your quantity is available prior to placing an order.
- Branded Products: allow 10 business days from proof approval for production. Branding options may be limited or unavailable based on product design or cover artwork.
- Unbranded Products: allow 3-5 business days for shipping. All Unbranded items receive FREE ground shipping in the US. Inquire for international shipping.
- RETURNS/CANCELLATIONS: All orders, branded or unbranded, are NON-CANCELLABLE and NON-RETURNABLE once a purchase order has been received.
Product Details
Author:
Axel Liebscher, Christoph A. Heinrich
Format:
Paperback
Pages:
442
Publisher:
De Gruyter (April 9, 2018)
Language:
English
Audience:
Professional and scholarly
ISBN-13:
9780939950775
ISBN-10:
0939950774
Weight:
23.84oz
Dimensions:
9.06" x 6.1"
File:
TWO RIVERS-PERSEUS-Metadata_Only_Perseus_Distribution_Customer_Group_Metadata_20260407163711-20260408.xml
Folder:
TWO RIVERS
List Price:
$51.99
Country of Origin:
Germany
Series:
Reviews in Mineralogy & Geochemistry
As low as:
$49.39
Publisher Identifier:
P-PER
Discount Code:
H
Pub Discount:
35
Imprint:
De Gruyter
Overview
Volume 65 of Reviews in Mineralogy and Geochemistry attempts to fill this gap and to explicitly focus on the role that co-existing fluids play in the diverse geologic environments. It brings together the previously somewhat detached literature on fluid–fluid interactions in continental, volcanic, submarine and subduction zone environments. It emphasizes that fluid mixing and unmixing are widespread processes that may occur in all geologic environments of the entire crust and upper mantle. Despite different P-T conditions, the fundamental processes are analogous in the different settings.








