Phanerozoic evolution of the North American Cordillera; United States and Canada

JS Oldow, AW Bally, HGA Lallemant, WP Leeman - 1989 - pubs.geoscienceworld.org
The rediscovery of America by the Genovese Christopher Columbus and the conquest of
Mexico by the Spaniards was followed by a more gradual, but equally relentless, occupation of …

Rheology of the upper mantle: inferences from peridotite xenoliths

HGA Lallemant, JCC Mercier, NL Carter, JV Ross - Tectonophysics, 1980 - Elsevier
Stress estimates as a function of depth are obtained for peridotite xenoliths from the upper
mantle of three types of tectonic environments by applying revised recrystallizedgrain-size …

Two high-pressure–low-temperature serpentinite-matrix mélange belts, Motagua fault zone, Guatemala: a record of Aptian and Maastrichtian collisions

GE Harlow, SR Hemming, HGA Lallemant… - …, 2004 - pubs.geoscienceworld.org
Left-lateral motion along the North American–Caribbean plate boundary has juxtaposed two
high-pressure–low-temperature (HP-LT) belts from separate Cretaceous collisions. These …

Active displacement partitioning and arc-parallel extension of the Aleutian volcanic arc based on Global Positioning System geodesy and kinematic analysis

HGA Lallemant, JS Oldow - Geology, 2000 - pubs.geoscienceworld.org
Global Positioning System geodesy and structural analysis of parts of the Aleutian island
chain support the interpretation of forearc migration westward along right-lateral transcurrent …

Stress dependence of recrystallized-grain and subgrain size in olivine

JV Ross, HGA Lallemant, NL Carter - Tectonophysics, 1980 - Elsevier
New experiments on Mt. Burnet dunite have been carried out to evaluate the effects of important
physical parameters on recrystallized-grain size and subgrain size in olivine deforming …

Slip and the clinoenstatite transformation as competing rate processes in enstatite

CB Raleigh, SH Kirby, NL Carter… - Journal of …, 1971 - Wiley Online Library
Previous experimental deformation of orthorhombic enstatite at temperatures from 200 to
1000C has produced clinoenstatite; yet, the natural occurrences of clinoenstatite in deformed …

Mechanisms of preferred orientations of olivine in tectonite peridotite

HGA Lallemant - Geology, 1975 - pubs.geoscienceworld.org
Preferred orientations of olivine have been produced by syntectonic recrystallization in
dunite samples that have been deformed moderately in a general stress field at high …

Metamorphic reworking of a high pressure–low temperature mélange along the Motagua fault, Guatemala: a record of Neocomian and Maastrichtian transpressional …

HK Brueckner, HGA Lallemant, VB Sisson… - Earth and Planetary …, 2009 - Elsevier
The Guatemala suture zone is a major east–west left-lateral strike slip boundary that separates
the North American and Caribbean plates in Guatemala. The Motagua fault, the central …

Displacement partitioning and arc-parallel extension in the Aleutian volcanic island arc

HGA Lallemant - Tectonophysics, 1996 - Elsevier
Convergence between the Pacific and North American plates along the Aleutian volcanic
island arc is generally right-oblique; the obliquity increases from 0 in the east to nearly 90 in …

[PDF][PDF] Pressure dependence of quartz deformation lamellae orientations

HGA Lallemant, NL Carter - American Journal of Science, 1971 - ajsonline.org
Experiments on Canyon Creck quartzite have been conducted at a constant strain rate of 78•
10 “/sec in the temperature range 6009 to 1050 C and confining pressure interval 4 to 20 kb …