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Ruiz Peak

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Journal Article
Published: 01 October 2011
European Journal of Mineralogy (2011) 23 (5): 703–715.
...Isabella Pignatelli; Massimo Nespolo Abstract The coexistence of two types of layer ( M 1 and M 2, differing for the origin in the octahedral sheet) in a mica polytype is confirmed for the first time in this work. The sample analysed is a 5-layer ferriphlogopite from the Ruiz Peak volcano...
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Journal Article
Published: 01 January 2011
European Journal of Mineralogy (2011) 23 (1): 73–84.
...Isabella Pignatelli; Michal Dusek; George De Titta; Massimo Nespolo Abstract The first reliable structural refinement of a non-MDO mica polytype from single-crystal X-ray diffraction data is presented. The sample is a 4-layer ferriphlogopite from the Ruiz Peak volcano, New Mexico, with cell...
FIGURES
Journal Article
Published: 01 November 2001
European Journal of Mineralogy (2001) 13 (6): 1047–1056.
...Massimo NESPOLO; Yoshihiro KUWAHARA Abstract An example of apparent polytypism in micas, i.e. twinning of a polytype giving a diffraction pattern which simulates that of a different polytype with longer periodicity, is reported from the Ruiz Peak ferric phlogopite, which is well known for the large...
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Image
(a) TMAFM amplitude image of the surface of the Ruiz Peak ferric phlogopite. (b) An enlarged, illuminated TMAFM height image of (a) (Z = 600 Å). Arrow A correspondants to that in (c) and (d), showing the front of the step of a single unit cell mica layer, (c) A cross-sectional view along line a-a’ in (b). Each step has a height af about 10Å, (d) An enlarged TMAFM height image of the part within the black box in (b) (Z = 200Å). (e) A height histogram of the data points within the white box in (d), showing that the step has a height of 10Å.
Published: 01 November 2001
Fig. 7. (a) TMAFM amplitude image of the surface of the Ruiz Peak ferric phlogopite. (b) An enlarged, illuminated TMAFM height image of (a) (Z = 600 Å). Arrow A correspondants to that in (c) and (d), showing the front of the step of a single unit cell mica layer, (c) A cross-sectional view along
Journal Article
Published: 01 March 2001
American Mineralogist (2001) 86 (3): 336–340.
...Toshihiro Kogure; Massimo Nespolo Abstract Atomic structures of planar defects found in oxybiotite from the Ruiz Peak ash flow, Jemez Mountains, New Mexico, were investigated using high-resolution transmission electron microscopy (HRTEM) and electron nano-beam chemical analyses. Two kinds of planar...
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Journal Article
Published: 01 February 2001
Clays and Clay Minerals (2001) 49 (1): 1–23.
... of inhomogeneous polytypes of titaniferous oxybiotite from Ruiz Peak (a volcanic environment where many inhomogeneous polytypes have been reported) are presented. Crystal Growth Long-Period Polytypes Mica Polytypism Figure 1. The structure of 1 M mica projected along the b axis. Closed...
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Journal Article
Published: 01 December 1975
American Mineralogist (1975) 60 (11-12): 1030–1040.
...Hiroshi Takeda; Malcolm Ross Abstract Crystal-structure analysis of coexisting 1 M and 2 M 1 biotite polytypes from a rhyodacite lava flow, Ruiz Peak, New Mexico, shows that the two forms possess essentially identical unit-cell parameters (in the 1 M setting), bond length averages, and site...
Image
Seismological context of north central Chile. Vertical lines represent the rupture length of major interplate earthquakes. Lines correspond to giant megathrust and recent earthquakes (Ruiz and Madariaga, 2018). Iso‐contours correspond to the slip in meters of Illapel rupture zone (Ruiz et al., 2016). Stars denote the epicenter of the Coquimbo 2019, Punitaqui 1997, and Tongoy 2013 earthquakes. Cyan inverted triangles mark the local strong‐motion stations, red inverted triangles correspond to regional strong‐motion stations, and dotted triangles are stations used in the section record of Figure 2. Vectors on stations are north and east peak ground acceleration, with the largest being 0.56g at station C10O. (Inset) Global map with the specified study area. The color version of this figure is available only in the electronic edition.
Published: 07 August 2019
Figure 1. Seismological context of north central Chile. Vertical lines represent the rupture length of major interplate earthquakes. Lines correspond to giant megathrust and recent earthquakes ( Ruiz and Madariaga, 2018 ). Iso‐contours correspond to the slip in meters of Illapel rupture zone
Image
Time scale ratio U/C against lahar Froude number for lahar monitoring sites at Nevado del Ruiz (NDR), Colombia (Pierson et al., 1990), Mount Saint Helens (MSH), United States (Pierson and Scott, 1985; Dinehart, 1999), and Mount Ruapehu, New Zealand (Cronin et al., 1999). Values of lahar hydraulic radius R used in calculations of Fr represent the intermediate hydraulic radius between hydraulic radius of the river h and hydraulic radius of the lahar at peak discharge. Linear functions through the origin delimit constant values of relative efficiency of bow-wave formation e in percent, because e = qBW/qL = Uh/UR.
Published: 01 May 2012
Figure 5. Time scale ratio U / C against lahar Froude number for lahar monitoring sites at Nevado del Ruiz (NDR), Colombia ( Pierson et al., 1990 ), Mount Saint Helens (MSH), United States ( Pierson and Scott, 1985 ; Dinehart, 1999 ), and Mount Ruapehu, New Zealand ( Cronin et al., 1999
Image
(A) Histogram of single-stage hafnium depleted mantle model ages (Hf TDM) of Red Bluff Granite Suite (RBGS) and other 1.1 Ga igneous and metamorphic rocks throughout Grenville Front. Model ages for these 1.1 Ga rocks were calculated by using Hf isotopic data reported by Howard (2013) and in this study. AppGn—Appalachian gneisses; CA-NV—California and southern Nevada; LU—Llano Uplift granitoids; NSEG—northern Sonora (Mexico) Escuadra granites; PP—Pikes Peak batholith (Colorado). (B) Histogram of Nd depleted mantle model ages (Nd TDM) of RBGS, Llano area, and Van Horn region rocks from Patchett and Ruiz (1989). Ages shown in parentheses correspond to the timing of emplacement of igneous and metamorphic rocks. LUG—Llano area post-collision granitoids; LUMR—Llano area metamorphic rocks (1.25–1.23 Ga), Van—Van Horn area.
Published: 01 February 2023
) and in this study. AppGn—Appalachian gneisses; CA-NV—California and southern Nevada; LU—Llano Uplift granitoids; NSEG—northern Sonora (Mexico) Escuadra granites; PP—Pikes Peak batholith (Colorado). (B) Histogram of Nd depleted mantle model ages (Nd T DM ) of RBGS, Llano area, and Van Horn region rocks from
Journal Article
Published: 01 February 2012
American Mineralogist (2012) 97 (2-3): 430–439.
... rock sample. Takeda and Ross (1975) , analyzed 2 M 1 and 1 M igneous oxybiotite from Ruiz Peak (New Mexico), and concluded that the unit layer of the 2 M 1 polytype showed a shift of the upper and lower triads of octahedral O atoms along the ± b direction with respect to the 1 M polytype...
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Journal Article
Published: 13 December 2024
The Seismic Record (2024) 4 (4): 318–326.
..., are common near volcanoes with intermittent explosions that generate strong airwaves. Reports of broken windows 7 km from Tungurahua Volcano, Ecuador ( Ruiz et al. , 2006 ) were common in 2006 and were coincident with audible blasts, referred to as cañonazos (Spanish) or cannon shots (M. Ruiz, personal comm...
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Journal Article
Published: 16 October 2024
Seismological Research Letters (2025) 96 (2A): 949–967.
... during explosive periods at Tungurahua ( Ruiz et al. , 2006 ; Matoza et al. , 2009 ; Fee et al. , 2010 ; Anderson et al. , 2018 ). Figure 3. 20 s samples of some repeating acoustic events indexed in the manual catalog as recorded in BMAS (unfiltered). P2PPr, peak‐to‐peak pressure...
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Journal Article
Published: 01 August 2021
Earthquake Spectra (2021) 37 (3): 1758–1784.
... of the results of nonlinear time history analysis. The statistical results reveal that the residual-to-peak-inelastic displacement ratios have the advantages of small dispersion, samples without any outliers, and relatively symmetric distribution, which benefits from the strong correlation between residual...
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Journal Article
Published: 01 October 2000
Clays and Clay Minerals (2000) 48 (5): 586–592.
...María Dolores Ruiz Cruz; Francisco Franco Abstract The intercalation complex of a low-defect dickite from Tarifa, Spain, with hydrazine was studied by high-temperature X-ray diffraction (HTXRD), differential thermal analysis (DTA), and thermogravimetry (TG). The X-ray diffraction (XRD) pattern...
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Book Chapter

Author(s)
Pilar Aranda
Series: Clay Minerals Society Workshop Lectures
Published: 01 January 2007
DOI: 10.1346/CMS-WLS-15.6
EISBN: 9781881208358
... functionalities such as electrical conductivity, insulating capacity, membrane effects, corrosion protection or fire retardant behavior ( Pinnavaia and Beall, 2000 ; Ruiz-Hitzky and Van Meerbeek, 2006 ). Among these, CPN that contain electroactive polymers with electronic conductivity, such as polyaniline (PANI...
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Journal Article
Published: 01 February 2022
Clays and Clay Minerals (2022) 70 (1): 48–61.
... ferriphlogopite from the Ruiz Peak (New Mexico, USA): First occurrence of a mica polytype with coexistence of M1- and M2- layers . European Journal of Mineralogy , 23 , 703 – 715 . Pignatelli , I. , Dusek , M. , De Titta , G. , & Nespolo , M. ( 2011 ). Structural modelling...
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Image
Published: 01 April 2011
. Zollo A. ( 2008 ). A Bayesian approach to the real-time estimation of magnitude from the early P and S wave displacement peaks , J. Geophys. Res. 113 , no.  B12302 , doi  10.1029/2007JB005386 . Lancieri M. Fuenzalida M. Ruiz S. Madariaga R. ( 2009 ). Magnitude
Journal Article
Published: 14 February 2018
Seismological Research Letters (2018) 89 (2A): 512–518.
...F. Leyton; C. Pastén; S. Ruiz; B. Idini; F. Rojas ABSTRACT The National Seismological Center of the University of Chile (CSN, Centro Sismológico Nacional) has been operating more than 400 seismic stations throughout the country. The data collected from this network, from March 2012 to August 2017...
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Journal Article
Published: 13 November 2019
Seismological Research Letters (2020) 91 (1): 262–271.
...Sebastián Carrasco; Sergio Ruiz; Miguel Sáez Abstract The Juan Fernandez Islands (JFI) are located in the Pacific Ocean 675 km west of the Chilean coast. This archipelago has historically been affected by large tsunamis. Robinson Crusoe Island (RCI), the main island of the JFI, was first inhabited...
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