English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Poster Abstract Field-based studies of exhumed faults have provided valuable insight into the structural geometry and rock textures of fault systems, yet few studies have examined a vertical, subsurface profile through a low-angle normal fault (LANF) system. Seismic reflection data from near the Department of Energy’s Frontier Observatory for Research in Geothermal Energy (FORGE) site to the west of the Mineral Mountains, UT, reveal a low-angle, W-dipping reflector underlying the basin fill. This surface is thought to represent a LANF, but its exact structural significance is still unclear. A Formation Microimager was logged in a vertical, 8.75 inch borehole over 2240-7550 ft in the Roosevelt Hot Springs Well 58-32 within the FORGE site, providing an “outcrop view” of the basin alluvium, igneous basement rock fabrics, and the textures and structures of this LANF system.

AN IMAGE LOG-BASED GEOMETRICAL AND TEXTURAL ANALYSIS OF A LOW-ANGLE NORMAL FAULT SYSTEM BENEATH THE F.O.R.G.E. SITE NEAR THE MINERAL MOUNTAINS, UTAH