The Textures of Rocks in the Earth’s Deep Interior: Part I. Understanding Anisotropy and Textures in Earth Materials ☆

Author(s):  
H.-R. Wenk ◽  
J. Gómez Barreiro ◽  
J.M. Benítez Pérez
Keyword(s):  
Author(s):  
Paolo Dulio ◽  
Andrea Frosini ◽  
Simone Rinaldi ◽  
Lama Tarsissi ◽  
Laurent Vuillon

AbstractA remarkable family of discrete sets which has recently attracted the attention of the discrete geometry community is the family of convex polyominoes, that are the discrete counterpart of Euclidean convex sets, and combine the constraints of convexity and connectedness. In this paper we study the problem of their reconstruction from orthogonal projections, relying on the approach defined by Barcucci et al. (Theor Comput Sci 155(2):321–347, 1996). In particular, during the reconstruction process it may be necessary to expand a convex subset of the interior part of the polyomino, say the polyomino kernel, by adding points at specific positions of its contour, without losing its convexity. To reach this goal we consider convexity in terms of certain combinatorial properties of the boundary word encoding the polyomino. So, we first show some conditions that allow us to extend the kernel maintaining the convexity. Then, we provide examples where the addition of one or two points causes a loss of convexity, which can be restored by adding other points, whose number and positions cannot be determined a priori.


2019 ◽  
Vol 116 (39) ◽  
pp. 19324-19329 ◽  
Author(s):  
Rajkrishna Dutta ◽  
Eran Greenberg ◽  
Vitali B. Prakapenka ◽  
Thomas S. Duffy

Neighborite, NaMgF3, is used as a model system for understanding phase transitions in ABX3 systems (e.g., MgSiO3) at high pressures. Here we report diamond anvil cell experiments that identify the following phases in NaMgF3 with compression to 162 GPa: NaMgF3 (perovskite) → NaMgF3 (post-perovskite) → NaMgF3 (Sb2S3-type) → NaF (B2-type) + NaMg2F5 (P21/c) → NaF (B2) + MgF2 (cotunnite-type). Our results demonstrate the existence of an Sb2S3-type post-post-perovskite ABX3 phase. We also experimentally demonstrate the formation of the P21/c AB2X5 phase which has been proposed theoretically to be a common high-pressure phase in ABX3 systems. Our study provides an experimental observation of the full sequence of phase transitions from perovskite to post-perovskite to post-post-perovskite followed by 2-stage breakdown to binary compounds. Notably, a similar sequence of transitions is predicted to occur in MgSiO3 at ultrahigh pressures, where it has implications for the mineralogy and dynamics in the deep interior of large, rocky extrasolar planets.


Physics Today ◽  
1992 ◽  
Vol 45 (3) ◽  
pp. 66-67
Author(s):  
Jean‐Paul Poirier ◽  
J. Michael Brown
Keyword(s):  

2004 ◽  
Vol 31 (2-3) ◽  
pp. 367-388 ◽  
Author(s):  
Christiane Schlaps

Summary The so-called ‘genius of language’ may be regarded as one of the most influential, and versatile, metalinguistic metaphors used to describe vernacular languages from the 17th century onwards. Over the centuries, philosophers, grammarians, trans­lators and language critics etc. wrote of the ‘genius of language’ in a wide range of text types and with reference to various linguistic positions so that a set of rather diverse types of the concept was created. This paper traces three prominent stages in the development of the ‘genius of language’ argument and, by identifying some of the most frequent types as they evolved in the context of the various linguistic dis­courses, endeavours to show the major transformations of the concept. While early on, discussion of the stylistic and grammatical type of the ‘genius of language’ concentrates on surface features in the languages considered, during the middle of the 18th century, the ‘genius of language’ is relocated to the semantic, interior part of language. With the 19th-century notion of an organological ‘genius of language’, the former static concept is personified and recast in a dynamic form until, taken to its nationalistic extremes, the ‘genius of language’ argument finally ceases to be of any epistemological and scientific value.


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