Strike-slip faulting in the core of the Central Range of west New Guinea: Ertsberg Mining District, Indonesia

2004 ◽  
Vol 116 (3) ◽  
pp. 277 ◽  
Author(s):  
Benyamin Sapiie ◽  
Mark Cloos
Geology ◽  
2005 ◽  
Vol 33 (8) ◽  
pp. 637-640 ◽  
Author(s):  
G. Gutiérrez-Alonso ◽  
J. Fernández-Suárez ◽  
Alan S. Collins ◽  
I. Abad ◽  
F. Nieto

Abstract The 40Ar/39Ar age data on single detrital muscovite grains complement U-Pb zircon ages in provenance studies, as micas are mostly derived from proximal sources and record low-temperature processes. Ediacaran and Cambrian sedimentary rocks from northwest Iberia contain unmetamorphosed detrital micas whose 40Ar/39Ar age spectra suggest an Amazonian–Middle American provenance. The Ediacaran sample contained only Neoproterozoic micas (590–783 Ma), whereas the Cambrian sample contained three age groups: Neoproterozoic (550–640 Ma, Avalonian–Cadomian–Pan African), Mesoproterozoic- Neoproterozoic boundary (ca. 920–1060 Ma, Grenvillian-Sunsas), and late Paleoproterozoic (ca. 1580–1780 Ma, Rio Negro). Comparison of 40Ar/39Ar muscovite ages with published detrital zircon age data from the same formations supports the hypothesis that the Neoproterozoic basins of northwest Iberia were located in a peri-Amazonian realm, where the sedimentary input was dominated by local periarc sources. Tectonic slivering and strike-slip transport along the northern Gondwanan margin affected both the basins and fragments of basement that were transferred from Amazonian to northern African realms during the latest Neoproterozoic–earliest Cambrian. Exhumation and erosion of these basement sources caused shedding of detritus to the Cambrian basins, in addition to detritus sourced in the continental mainland. The apparent dominance of Rio Negro–aged micas in the Cambrian sandstone suggests the presence of unexposed basement of that age beneath the core of the Ibero-Armorican Arc.


2021 ◽  
Vol 21 (2) ◽  
pp. 3-18
Author(s):  
Lauro Cézar Montefalco de Lira Santos ◽  
Luís Gustavo Ferreira Viegas

We discuss meso- and microstructural features of granites closely related to strike-slip shear zones in the Borborema Province, NE Brazil. The Riacho do Icó stock is an en-cornue intrusion aged at ca. 607 Ma. Magmatic fabric is recorded in the core of the granite, whilst increasing deformation is marked by the development of mylonitic fabrics towards the Afogados da Ingazeira shear zone, including magmatic foliation and lineation rotation. Early recrystallization of quartz and K-feldspar crystals is widespread as a fabric with well-developed granoblastic polygonal textures and lobate subgrain boundaries, heterogeneously deformed lenses and ameboid quartz ribbons, typical of igneous rocks submitted to deformation in deep crustal levels. On the other hand, the Espinho Branco-Santa Luzia leucogranitic belt is hosted along the Patos Lineament, aged between the ca. 575 – 565 Ma interval. These rocks show discordant relationships with the host migmatites and the main deformational fabric is characterized by a dominant magmatic foliation that is locally overprinted by structures that are typical of solid-state flow. Quartz melt pockets and interstitial quartz grains filling fractures in feldspar clasts are common. Such characteristics are compatible with granites that were injected in the continental crust along planar anisotropies (i.e., shear zones) formed during the late-stage partial melting events that originated the migmatites of the area. The case studies are proxies in the understanding of different episodes of magma emplacement along shear zones in this part of West Gondwana.


1995 ◽  
Vol 8 (1) ◽  
pp. 57 ◽  
Author(s):  
LD Pryor ◽  
ER Williams ◽  
BV Gunn

Over 400 specimens from 26 locations, mainly in the Lesser Sunda Islands and some from New Guinea and northern Cape York, were examined. These were representative of an array of forms ordinarily assigned to Eucalyptus urophylla, E. pellita and an undescribed species as well as those considered by some to be hybrid between E. alba and E. urophylla. The latter has long been considered to show considerable polymorphism. Re-examination of the available material and records suggest that interspecific hybridisation is not significantly involved in this variability. Although this examination pointed to the existence of some differentiation at the level of species in this array, there was still a core of material which could not be separated readily into subgroups. Measurements were taken of selected floral and foliar morphological features which were then subject to statistical analysis to ascertain if subgroups were discernible on this basis. As a result, the separation of two species, Eucalyptus orophila sp. nov. and Eucalyptus wetarensis sp. nov. from Eucalyptus urophylla sensu lato in the Lesser Sunda Islands, is supported. The related populations called species A by Pinyopusarerk et al. (1993), from New Guinea and northern Cape York, were to a somewhat lesser extent separated on these criteria. These results were paralleled by evidence from seedling morphology and oil characteristics. Isozyme analysis gave a similar grouping for the material from Wetar, but did not indicate other separations from the core E. urophylla.


2004 ◽  
Vol 45 (2) ◽  
pp. 271-274 ◽  
Author(s):  
Richard Schechner

Frankly, I'm not much of a historian. That is, the past interests me mostly as grist for my theoretical mill. I am not nostalgic. I don't often trek through ruins—whether of stone, paintings, videotape, paper, library stacks, or my own many notebooks. Of course, I've done the right thing when it comes to this kind of activity. I have climbed the pyramids at Teotihuacan and in Mayan country, sat on stone benches of the Theatre of Dionysus in Athens and in Epidaurus (where I was tormented by some really awful productions of ancient Greek dramas), and visited the theatre museums of four continents. On the art-history front, I've gazed at more paintings and sculptings than I can readily organize in memory. But my strongest meetings with “history” have been at the cusp of the past and present—living events always already changing as they are (re)performed. This has been the core of my “anthropology-meets-theatre” work whether among the Yaquis of Arizona, at the Ramlila of Ramnagar in India, in the highlands of Papua–New Guinea, at Off-Off Broadway in New York, in the interior of China, and at very many other events in a wide variety of places.


2021 ◽  
pp. 1-15
Author(s):  
Deepak C. Srivastava ◽  
Ajanta Goswami ◽  
Amit Sahay

Abstract Delimiting the Aravalli mountain range in the east, the Great Boundary Fault (GBF) occurs as a crustal-scale tectonic lineament in the NW Indian Shield. The structural and tectonic characteristics of the GBF are, as yet, not well-understood. We attempt to fill this gap by using a combination of satellite image processing, high-resolution outcrop mapping and structural analysis around Chittaurgarh. The study area exposes the core and damage zone of the GBF. Three successive phases of folding, F1, F2 and F3, are associated with deformation in the GBF. The large-scale structural characteristics of the GBF core are: (i) a non-coaxial refolding of F1 folds by F2 folds; and (ii) the parallelism between the GBF and F2 axial traces. In addition, numerous metre-scale ductile shear zones cut through the rocks in the GBF core. The damage zone is characterized by the large-scale F1 folds and the mesoscopic-scale strike-slip faults, thrusts and brittle-ductile shear zones. Several lines of evidence, such as the inconsistent overprinting relationship between the strike-slip faults and thrusts, the occurrence of en échelon folds and the palaeostress directions suggest that the GBF is a dextral transpression fault zone. Structural geometry and kinematic indicators imply a wrench- and contraction-dominated deformation in the core and damage zone, respectively. We infer that the GBF is a strain-partitioned dextral transpression zone.


2021 ◽  
Author(s):  
Derek Neuharth ◽  
et al.

Description of the model setup (including governing and rheologic equations) and coupling between codes FastScape and ASPECT in more detail, and supplemental figures with additional information including mapviews of the New Guinea, Yinggehai, and Navassa Basins.<br>


2018 ◽  
Vol 22 (3) ◽  
pp. 437-494 ◽  
Author(s):  
Antoinette Schapper ◽  
Lourens de Vries

Abstract Using a sample of 116 languages, this article investigates the typology of comparative constructions and their distribution in Melanesia, one of the world’s least-understood linguistic areas. We present a rigorous definition of a comparative construction as a “comparative concept”, thereby excluding many constructions which have been considered functionally comparatives in Melanesia. Conjoined comparatives are shown to dominate at the core of the area on the island of New Guinea, while (monoclausal) exceed comparatives are found in the maritime regions around New Guinea. Outside of Melanesia adpositional and other comparative constructions including particle comparatives are most frequent in Austronesian languages. The unity of the conjoined comparative type in the core Melanesian area illustrates that, while morpho-syntactic profiles of Melanesian languages are heterogenous, significant convergence in the “ways of saying things” can be found across the region. Additionally, we find no cases of clause chaining constructions being used for encoding comparatives, even in canonical clause chaining languages of central New Guinea. Our findings thus offer no support for Stassen’s claim of a correlation between temporal chaining type and comparative construction type. Instead we suggest that an areal preference for mini-clauses may explain the dominance of the conjoined comparative in Melanesia.


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