Coca’s haunting presence in the agrarian politics of the Bolivian lowlands     

Gabriela Valdivia 《GeoJournal》2012,77(5):615-631

This essay explores the role of the coca economy in the politics of basic foodstuff production in the lowlands department of Santa Cruz, Bolivia. Efforts throughout the 1980s and 1990s to diminish the coca economy in Santa Cruz have led to a significant decrease in the physical presence of coca in the region. This paper argues that while coca has been physically eradicated, the relationships and inequalities that characterized the coca economy at its height in the 1980s and 1990s continue to haunt present-day agrarian relations and decisions in the region. Using the framework of haunting and drawing on stories narrating the intersections between the livelihood challenges of rice farmers in the province of Ichilo, Santa Cruz, regional agrarian politics, and regional-state governance conflicts, I explore how the coca economy matters to the dynamics of principal agrarian foodstuff production. While coca cultivation in Ichilo is expressly assigned to the past and modern agrarian politics are explicitly articulated as “post-coca,” this paper offers a reminder about how the coca economy continues to shape present day agrarian politics, even as it is considered “successfully” eradicated.  相似文献   

Historical intensity VIII earthquakes along the Rhone valley (Valais, Switzerland): primary and secondary effects     

Stefan Fritsche  Donat F?h  Gabriela Schwarz-Zanetti 《Swiss Journal of Geoscience》2012,105(1):1-18

In recent years the upper Rhone Valley has been one of the most intensively investigated regions by the Swiss Seismological Service. The high seismicity in the region encourages research in the seismological field and one main focus has been historical seismology. This report presents the state of the art of our historical investigations by giving an overview of the effects of four damaging earthquakes with intensity larger than VII, for which a fairly large number of documents could be found and analyzed. The overview includes the events of 1584 (Aigle, epicentral intensity VIII), 1755 (Brig, epicentral intensity VIII), 1855 (Visp, epicentral intensity VIII), and 1946 (Sierre, epicentral intensity VIII for the main shock and intensity VII for the largest aftershock). The paper focuses mainly on primary and secondary effects in the epicentral region, providing the key data and a general characterization of the event. Generally, primary effects such as the reaction of the population and impact on buildings took more focus in the past. Thus building damage is more frequently described in historic documents. However, we also found a number of sources describing secondary effects such as landslides, snow avalanches, and liquefaction. Since the sources may be useful, we include citations of these documents. The 1584 Aigle event, for example, produced exceptional movements in Lake Geneva, which can be explained by an expanded sub aquatic slide with resultant tsunami and seiche. The strongest of the aftershocks of the 1584 event triggered a destructive landslide covering the villages Corbeyrier and Yvorne, VD. All macroseismic data on the discussed events are accessible through the webpage of the Swiss Seismological Service (http://www.seismo.ethz.ch).  相似文献   

Applying GNSS and DTM Technologies to Monitor the Ice Balance of the Horcones Inferior Glacier, Aconcagua Region, Argentina     

M. Gabriela Lenzano  Luis Lenzano  Darío Trombotto Liaudat  Jorge Barón  Esteban Lannutti 《Journal of the Indian Society of Remote Sensing》2013,41(4):969-980

This work provides results and analysis of the behavior in a reconstituted debris covered glacier, Horcones Inferior (HIG). This glacier is located at 32° 41′ S and 69° 57′ W in the Aconcagua region, Mendoza, Argentina. The HIG has experienced surges events in 1984 and 2003. GNSS techniques and Digital Terrain Models (DTMs) derived from ASTER optical imagery, were used to detect movements and altimetric changes of the HIG in the 2001–2012 period. Based on a GNSS semi - continuous station, N and E mean velocities of 0.9 cm/d and 1.1 cm/d and in U direction were 1.1 cm/d and 1.5 cm/d were obtained respectively in 2009–2010 period. Additionally, GNSS profiles showed a velocity range between 0.5 cm/d and 2.8 cm/d. Finally, through a DTM comparison the altimetric change before and after the last surge in 2003 was obtained. The applied techniques allowed accurate and reliable change detection of the HIG.  相似文献   

Deformation and metamorphism in the Fenes Nappe (southern Apuseni Mountains,Romania)Déformation et métamorphisme dans la nappe de Fenes (monts Apuseni méridionaux,Roumanie)     

Alessandro Ellero  Leonardo Leoni  Michele Marroni  Ionel Nicolae  Luca Pandolfi  Franco Sartori 《Comptes Rendus Geoscience》2002,334(5):347-354

The Fenes Nappe belongs to the stack of tectonic units cropping out in the southern Apuseni Mts (Romania). It is characterised by a structural history consisting of two folding phases that developed during the time spanning from Early Aptian to Late Maastrichtian. The D1 phase produced west-northwest-verging, isoclinal to very tight folds, associated to a slaty cleavage. The main metamorphic imprint of the Fenes Nappe is linked to this deformation phase; illite and chlorite ‘crystallinity’ values indicate metamorphic conditions of the late diagenesis, close to the diagenetic zone/anchizone boundary. The subsequent D2 phase produced north-northwest-verging, parallel folds, not associated with synkinematic recrystallisation. These phases are interpreted as developed during a structural path, which includes burial at a depth of 8–10 km, followed by exhumation at shallower structural levels. To cite this article: A. Ellero et al., C. R. Geoscience 334 (2002) 347–354.  相似文献   

The geology of the Oceanographer Transform: The ridge-transform intersection     

J. A. Karson  P. J. Fox  H. Sloan  K. T. Crane  W. S. F. Kidd  E. Bonatti  J. B. Stroup  D. J. Fornari  D. Elthon  P. Hamlyn  J. F. Casey  D. G. Gallo  D. Needham  R. Sartori  OTTER 《Marine Geophysical Researches》1984,6(2):109-141

Seven dives in the submersible ALVIN and four deep-towed (ANGUS) camera lowerings have been made at the eastern ridge-transform intersection of the Oceanographer Transform with the axis of the Mid-Atlantic Ridge. These data constrain our understanding of the processes that create and shape the distinctive morphology that is characteristic of slowly-slipping ridge-transform-ridge plate boundaries. Although the geological relationships observed in the rift valley floor in the study area are similar to those reported for the FAMOUS area, we observe a distinct change in the character of the rift valley floor with increasing proximity to the transform. Over a distance of approximately ten kilometers the volcanic constructional terrain becomes increasingly more disrupted by faulting and degraded by mass wasting. Moreover, proximal to the transform boundary, faults with orientations oblique to the trend of the rift valley are recognized. The morphology of the eastern rift valley wall is characterized by inward-facing scarps that are ridge-axis parallel, but the western rift valley wall, adjacent to the active transform zone, is characterized by a complex fault pattern defined by faults exhibiting a wide range of orientations. However, even for transform parallel faults no evidence for strike-slip displacement is observed throughout the study area and evidence for normal (dip-slip) displacement is ubiquitous. Basalts, semi-consolidated sediments (chalks, debris slide deposits) and serpentinized ultramafic rocks are recovered from localities within or proximal to the rift valley. The axis of accretion-principal transform displacement zone intersection is not clearly established, but appears to be located along the E-W trending, southern flank of the deep nodal basin that defines the intersection of the transform valley with the rift floor.  相似文献   

Microseismicity, tectonics and seismic potential in southern Caribbean and northern Venezuela     

Omar J. Pérez  Carlos Sanz  Gabriela Lagos 《Journal of Seismology》1997,1(1):15-28

Approximately one thousand microearthquakes with body-wave magnitude mb have been located in northern Venezuela and the southern Caribbean region (9–12° N; 64–70° W) since the installation in 1980 of the Venezuelan Seismological Array, together with forty events of mb 4, one of them with surface-wave magnitude Ms 6. Focal depths are in the range of 0 to <15 km. This geologically complex region is part of the boundary between the Caribbean and the South American Plates. Epicentral locations indicate that this E–W oriented portion of the boundary is formed by two 400 km long subparallel fault zones: San Sebastián fault zone (SSF), 20 km north of Caracas along the coast; and La Victoria fault zone (LVF), 25 km south of the city. They are clearly delineated by the microseismicity. New composite focal mechanism solutions (CFMS) along these faults show right-lateral strike-slip (RLSS) motion on nearly E–W oriented fault planes. NW-striking subsidiary active faults occur in the region and intercept the two main E–W fault zones. These interceptions show high levels of microearthquake activity and seismic moment release when compared to other portions of both, the main and subsidiary faults. New CFMS at those fault crossing sites show NW-striking RLSS motion and normal faulting, in an en-echelon-like structural behavior. Geological data and quantitative comparisons with other transcurrent plate boundaries in the world suggest that the rate of plate motion in this area is on the order of 20 mm/y. Several moderate and large shocks have occurred along the SSF and LVF since 1640, including an Ms 7.6 event in 1900 on SSF. Although the region may be relatively far from a repeat of this earthquake, seismicity data indicate that strong shocks could take place along segments of the seismically active faults identified in this study.  相似文献   

Late Miocene calc-alkalic volcanism in northwestern Mexico: an expression of rift or subduction-related magmatism?     

Gabriela Mora-Klepeis  Fred W. McDowell 《Journal of South American Earth Sciences》2004,17(4):292

Magmatism in NW Mexico records a Late Miocene transformation from convergence to extension in the Gulf of California rift system. Miocene calc-alkalic rocks in the Baja California peninsula are related to the final subduction of the Farallon plate system, but the heterogeneous nature of volcanism younger than 12.5 Ma has led to conflicting tectonic interpretations. Neogene volcanic rocks in the Sierra Santa Ursula, Sonora, were emplaced in three magma pulses, according to mapping, K–Ar geochronology, and geochemistry. From 23.5 to 15 and 14 to 11.4 Ma, calc-alkalic rocks show an arc-like signature. The 12–11 Ma calc-alkalic dacites, however, are characterized by higher K, Rb, ⁸⁷Sr/⁸⁶Sr, and light REE abundances than are the older rocks. The timing, petrography, and geochemistry of the 12–11 Ma rocks are interpreted to reflect postsubduction magmatism. A change in magma chemistry from predominantly calc-alkalic to tholeiitic rocks at 10.3 Ma corresponds to orthogonal extension during early Gulf of California evolution. Sr, Nd, and Pb radiogenic isotope signatures show minor changes over time. The volcanic record for 20–12.5 Ma at Sierra Santa Ursula and adjacent areas is consistent with the reconstructed history of the Guadalupe microplate. The interval of magmatism produced from 12 to 11 Ma appears to reflect changes in plate geometry during the transition from subduction to rifting.  相似文献   

The crystal structure of a 1M lepidolite     

Dr. F. Sartori 《Mineralogy and Petrology》1976,23(1):65-75

Summary The crystal structure of a 1M lepidolite coexisting with the 2M ₂ form, from the Island of Elba, Tuscany, Italy has been determined and refined by least-squares methods using three-dimensional data collected by the Weissenberg method with CuK radiation. The lattice parameters are:a=5.20(2),b=9.01(2),c=10.09(1) Å and =99.28°(33). The space group isC2/m. The final residual isR=6.7% using isotropic temperature factors. Comparison of the 1M lepidolite structure with that of the coexisting 2M ₂ polymorph shows the absence of significant differences both in chemical composition and in structural parameters; also for the 1M structure the main features are, in fact, a remarkable octahedral ordering and a considerable distortion of the tetrahedra joined with a relatively low ditrigonality (=7.41°) of their arrangement.

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Structure cristalline d'une lépidolite 1M

Résumé La structure cristalline d'une lépidolite 1M de l'Île d'Elbe, Toscane, Italie, coexistant dans le même échantillon avec le polymorphe 2M ₂, a été resolue et affinée par la methode des moindres carrés en utilisant les données recueillies à partir de clichés de Weissenberg, enregistrés sous rayonnement CuK. Les dimensions de la maille sont les suivantes:a=5.20(2),b=9.01(2),c=10.09(1) Å, =99.28°(33). Le groupe d'espace estC2/m. L'affinement de la structure en isotropie des facteurs d'agitation thermique a amené à une valeur finale du facteurR de 6.7%. En comparant la structure de la lépidolite 1M avec celle du polymorphe 2M ₂ présent dans le même échantillon on peut noter qu'il n'y a pas, pratiquement, des differences significatives entre les deux, soit en composition chimique soit en paramètres structuraux; en effet on remarque que la lépidolite 1M aussi est caractérisée par un considerable ordre dans la distribution des cations dans la couche octaèdrique, par une forte déformation des tetraèdres et par une faible déviation de l'héxagonalitè (=7.41°) de la disposition de ces dernier polyèdres.

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Variations in some physico-chemical parameters in a hypersaline coastal lagoon of Baja California,Mexico     

Gabriela Montaño Moctezuma  L. Fernando Bückle Ramírez 《International Journal of Salt Lake Research》1995,4(3):265-280

San Jose lagoon is a hypersaline body of water located in Mexico in the Baja California Peninsula. The lagoon belongs to a system that lies between the fault ridge known as San Jose Creek. Because of its marine origin, it can be considered as thalassohaline, but its isolation from the ocean has brought about changes in its salt composition. It has an area of 13,500 m², a mean depth of 80 cm and a total volume of 10,000 m³. It does not desiccate and can be considered as a permanent lagoon. Seasonal variations are small. TheArtemia population in San Jose produces cysts all year. To determine the physico-chemical conditions inducing permanent production of cysts, temperature, salinity, dissolved oxygen, and pH of the lagoon were monitored, as well as relative humidity and wind conditions in the region in different seasons of the year. From spring to summer, differences of 1 mg L^–1 of O₂, 1°C in water temperature, and 8 g L^–1 in salinity were observed, and from summer to winter differences of 3.3 mg L^–1, 6.5°C, and 14 g L^–1, respectively. Despite small seasonal variations, the lagoon exhibits strong spatial and daily changes that are important for cyst production.  相似文献   

A review of the tectonic evolution of the Sunsás belt,SW Amazonian Craton     

Wilson Teixeira  Mauro Cesar Geraldes  Ramiro Matos  Amarildo Salina Ruiz  Gerson Saes  Gabriela Vargas-Mattos 《Journal of South American Earth Sciences》2010,29(1):47-60

The Sunsás–Aguapeí province (1.20–0.95 Ga), SW Amazonian Craton, is a key area to study the heterogeneous effects of collisional events with Laurentia, which shows evidence of the Grenvillian and Sunsás orogens. The Sunsás orogen, characterized by an allochthonous collisional-type belt (1.11–1.00 Ga), is the youngest and southwesternmost of the events recorded along the cratonic fringe. Its evolution occurred after a period of long quiescence and erosion of the already cratonized provinces (>1.30 Ga), that led to sedimentation of the Sunsás and Vibosi groups in a passive margin setting. The passive margin stage was roughly contemporary with intraplate tectonics that produced the Nova Brasilândia proto-oceanic basin (<1.21 Ga), the reactivation of the Ji-Paraná shear zone network (1.18–1.12 Ga) and a system of aborted rifts that evolved to the Huanchaca–Aguapeí basin (1.17–1.15 Ga). The Sunsás belt is comprised by the metamorphosed Sunsás and Vibosi sequences, the Rincón del Tigre mafic–ultramafic sill and granitic intrusive suites. The latter rocks yield ε_Nd(t) signatures (?0.5 to ?4.5) and geochemistry (S, I, A-types) suggesting their origin associated with a continental arc setting. The Sunsás belt evolution is marked by “tectonic fronts” with sinistral offsets that was active from c. 1.08 to 1.05 Ga, along the southern edge of the Paraguá microcontinent where K/Ar ages (1.27–1.34 Ga) and the Huanchaca–Aguapeí flat-lying cover attest to the earliest tectonic stability at the time of the orogen. The Sunsás dynamics is coeval with inboard crustal shortening, transpression and magmatism in the Nova Brasilândia belt (1.13–1.00 Ga). Conversely, the Aguapeí aulacogen (0.96–0.91 Ga) and nearby shear zones (0.93–0.91 Ga) are the late tectonic offshoots over the cratonic margin. The post-tectonic to anorogenic stages took place after ca. 1.00 Ga, evidenced by the occurrences of intra-plate A-type granites, pegmatites, mafic dikes and sills, as well as of graben basins. Integrated interpretation of the available data related to the Sunsás orogen supports the idea that the main nucleus of Rodinia incorporated the terrains forming the SW corner of Amazonia and most of the Grenvillian margin, as a result of two independent collisional events, as indicated in the Amazon region by the Ji-Paraná shear zone event and the Sunsás belt, respectively.  相似文献