Sladen Fault

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Journal Article
Journal: Economic Geology
Published: 01 September 2019
Economic Geology (2019) 114 (6): 1057–1094.
... assemblage (<2680–2670 Ma in the southern Abitibi). The orebodies define two main mineralized trends, which are oriented subparallel to the NW-striking S 2 cleavage and the E-striking, S-dipping Sladen fault zone. This syn- to post-D 2 ductile-brittle to brittle Sladen fault zone is mineralized for more...
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Series: Society of Economic Geologists
Published: 01 January 2017
DOI: 10.5382/Rev.19.09
EISBN: 9781629491172
... is characterized by a Au-Te-W-S-Bi-Ag ± Pb ± Mo metallic signature, mainly consists of quartz-carbonate vein stockworks and replacement zones with disseminated pyrite. The ore zones are dominantly oriented subparallel to a NW-striking S 2 foliation and to the E-striking and S-dipping Sladen fault, thus forming NW...
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Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2020
DOI: 10.5382/SP.23.02
EISBN: 9781629496429
... associated with the Sladen fault and ~2678 Ma subalkaline to alkaline porphyritic quartz monzodiorite and granodiorite. Field relationships and isotopic age data for ore-related vein minerals indicate that gold mineralization in the Canadian Malartic deposit occurred at ~2665 to 2660 Ma...
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(A) Simplified geologic map of the <span class="search-highlight">Sladen</span> zone in the Canadian Malartic ope...
Published: 01 September 2019
Fig. 15. (A) Simplified geologic map of the Sladen zone in the Canadian Malartic open pit. Modified from De Souza et al. (20l7a). White arrows mark the approximate northern and southern limits and apparent width variations of the Sladen fault zone. (B) Detailed map of hydrothermal alteration
Photographs of hydrothermally altered quartz monzodiorite. (A) Calcite-hema...
Published: 01 September 2019
at outcrop showing veinlets with bleached selvages composed of carbonate-feldspar assemblage developed as a stockwork in surrounding calcitehematite assemblage, footwall of Sladen fault. (G) Carbonate-feldspar assemblage occurring as a decametric replacement zone, Sladen zone. Note the transition
Host rocks of the Canadian Malartic gold mine. (A) Graywacke with load stru...
Published: 01 September 2019
at the Sladen zone intrusion. The stippled lines highlight a S- to SE-dipping cleavage in the footwall of the Sladen fault. The dotted white box is for the location of the photograph shown in Figure 7E . (D) S 2 pressure solution cleavage, stratification, and E-plunging intersection lineation (white lines
(A) Simplified geologic map of the southeast extension of the Gilbert zone....
Published: 01 September 2019
alteration is invading the sedimentary rocks along most reactive layers. (D) Section of the East Malartic mine between ~ 730- and 1,100-m depth (adapted from Fallara et al., 2000 ). (E) Photograph looking east at the Sladen fault, Sladen zone. Gold grades in parts per million are indicated for the main ore
Conceptual model for the timing of gold mineralization at the Canadian Mala...
Published: 01 September 2019
of the Canadian Malartic deposit during (post-Timiskaming) D 2 deformation; grt = interpreted position of the garnet isograd. The main phase of hydrothermal alteration and gold mineralization is associated with the formation of brittle to brittle-ductile faults, including the Sladen fault, during late D 2
Photomicrographs of hydrothermally altered sedimentary rocks. (A, B) K-mica...
Published: 01 September 2019
plagioclase. (H) Backscattered microprobe image of K-feldspar-dolomite veinlet and K-feldspar replacing albite in carbonate-feldspar assemblage. (I) S-C deformation fabric marked by phlogopite, feldspar neoblasts, and carbonates, Sladen fault. Note the presence of fractured fish-shaped albite porphyroclast
Examples of range of outer-rise seismicity characteristics following large ...
Published: 06 July 2018
Figure 18. Examples of range of outer-rise seismicity characteristics following large and great megathrust earthquake ruptures, reprinted from Sladen and Trevisan (2018) , with permission from Elsevier. In several large to great earthquakes with slip distributions (green-blue shading) indicating
Finite <span class="search-highlight">fault</span> models for earthquakes recorded from Chilean stations         ...
Published: 01 November 2016
Table 1 Finite fault models for earthquakes recorded from Chilean stations EQID Earthquake name/year Primary choice Others 50001 Valparaiso/1985 Mendoza et al. (1994) 50003 Antofagasta/1995 Shao and Ji (UCSB) 50020 Southern Peru/2001 Shao and Ji (UCSB
Alternate finite-<span class="search-highlight">fault</span> models for 2010  M 8.81 Maule earthquake            ...
Published: 01 May 2022
Table 5. Alternate finite-fault models for 2010 M 8.81 Maule earthquake Model Automated (Y/N) Data sources Peer-review document (Y/N) Sladen (2010) Y Teleseismic N Hayes (2010 , 2017) Y (2010),N (2017a) Teleseismic N Luttrell et al. (2011) N Crustal
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2010
AAPG Bulletin (2010) 94 (11): 1695–1712.
..., and clastic margin studies. Many of Southeast Asia's largest oil and gas fields (e.g., Minas ∼4 × 10 9 bbl of oil) are found within the Paleogene nonmarine rifts of Indonesia, where production has been declining since 1993 ( Sladen, 1997a ; Doust and Sumner, 2007 ). Although the prolific nonmarine...
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Series: SEPM Gulf Coast Section Publications
Published: 01 December 2010
DOI: 10.5724/gcs.10.30.0376
EISBN: 978-0-9836096-0-5
... rocks are widespread in several rift petroleum systems, particularly in the Southeast Asia area ( Katz, 1995 ; Doust and Sumner, 2007 ; Doust and Nobel, 2008; Matthews et al ., 1997 ; Sladen, 1997b ). Nearer the faulted margin, the HAH facies becomes thicker and reflectors become stronger...
Journal Article
Published: 01 April 2022
Seismological Research Letters (2022) 93 (3): 1573–1584.
...Itzhak Lior; E. Diego Mercerat; Diane Rivet; Anthony Sladen; Jean‐Paul Ampuero Abstract Distributed acoustic sensing (DAS) is an ideal tool for ambient noise tomography owing to the dense spatial measurements and the ability to continuously record in harsh environments, such as underwater. Although...
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Journal Article
Journal: GSA Bulletin
Published: 01 December 2001
GSA Bulletin (2001) 113 (12): 1560–1579.
... basal alluvial and fluvial conglomerate to fluvial and lacustrine sandstone and mudstone. Resedimented ashes and basalt flows punctuate the synrift megasequence. Rifting began in the Unegt subbasin prior to 155 Ma with coarse alluvial filling of local fault depressions. Subsidence generally outstripped...
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