logo

EbookBell.com

Most ebook files are in PDF format, so you can easily read them using various software such as Foxit Reader or directly on the Google Chrome browser.
Some ebook files are released by publishers in other formats such as .awz, .mobi, .epub, .fb2, etc. You may need to install specific software to read these formats on mobile/PC, such as Calibre.

Please read the tutorial at this link:  https://ebookbell.com/faq 


We offer FREE conversion to the popular formats you request; however, this may take some time. Therefore, right after payment, please email us, and we will try to provide the service as quickly as possible.


For some exceptional file formats or broken links (if any), please refrain from opening any disputes. Instead, email us first, and we will try to assist within a maximum of 6 hours.

EbookBell Team

Basic Theory In Reflection Seismology Volume 1 With Mathematica Notebooks And Examples On Cdrom 1st Costain Jk

  • SKU: BELL-2269100
Basic Theory In Reflection Seismology Volume 1 With Mathematica Notebooks And Examples On Cdrom 1st Costain Jk
$ 31.00 $ 45.00 (-31%)

0.0

0 reviews

Basic Theory In Reflection Seismology Volume 1 With Mathematica Notebooks And Examples On Cdrom 1st Costain Jk instant download after payment.

Publisher: Elsevier
File Extension: PDF
File size: 30.16 MB
Pages: 576
Author: Costain J.K., Coruh C.
ISBN: 9780080370194, 0080370195
Language: English
Year: 2004
Edition: 1st

Product desciption

Basic Theory In Reflection Seismology Volume 1 With Mathematica Notebooks And Examples On Cdrom 1st Costain Jk by Costain J.k., Coruh C. 9780080370194, 0080370195 instant download after payment.

The material in this volume provides the basic theory necessary to understand the principles behind imaging the subsurface of the Earth using reflection and refraction seismology. For reflection seismology, the end product is a ''record section'' from a collection of ''wiggly traces'' that are recorded in the field from which information about the properties of subsurface structure and rock can be derived. For the most part, the principles of imaging are the same regardless of the depth to the target; the same mathematical background is necessary for targeting a shallow water table as for investigating the base of the earth's continental ''crust'' at a depth of 30-50 km.

Related Products