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On 25 February 1999, Guatemalans received the much anticipated report of the United Nations-sponsored Commission for Historical Clarification (CEH), Memory of Silence, which detailed wartime atrocities and decades-long American support of the Guatemalan army. This document followed the earlier release of the Catholic church's own REMHI report (Recuperation of Historical Memory Inter-diocesan Project), Guatemala: never again . Using the recently released reports and databases of the CEH and REMHI, we explore the significant use of testimonio as a tool of shared witnessing, collective remembrance, and individual recollection of the special brutality directed against Maya women. Through testimonio, the outcomes of visible and invisible terror and violence in Guatemala are articulated as personal, social and geographic spaces of terror, all of which are gendered and racialised. With the civil war officially over, Maya women of Guatemala see the spaces of terror diminish. Given debates over testimonio, however, the grounds for assault and denial remain fertile.  相似文献   
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This article studies employment location patterns in the Puget Sound Region of Washington State at a micro level of geography. Traditional discrete choice modeling using multinomial logit (MNL) models may be problematic at a micro level of geography due to the high dimensionality of the set of alternative locations and the likely violations of the independence from irrelevant alternatives (IIA) assumption. Count models are free from the IIA assumption and, unlike logit models, actually benefit from large numbers of alternatives by adding degrees of freedom. This study identifies the best-fitting count model as the zero-inflated negative binomial (ZINB) model, because this model more effectively addresses the large number of cells with no jobs and reflects a dual process that facilitates the identification of threshold clustering effects such as those found in specialized employment centers. The estimation and prediction results of ZINB are compared with those of MNL with a random sampling of alternatives estimated on an equivalent data set. The ZINB and MNL models largely agree on major trends, with the ZINB model providing more insightful details, but with less capacity to predict large count situations.  相似文献   
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ABSTRACT. This study develops a computable general equilibrium (CGE) model of California to examine the impact of recent defense cuts on the state's economy. The study demonstrates use of a CGE model to examine the sensitivity of regional economy models to assumptions about factor migration. Model variants include input-output and closed economy models as limiting cases. The results show that the California economy is sensitive to defense cuts. The multiplier relating the impact of defense cuts to state product ranges from one to almost five, depending on the degree of interstate factor mobility.  相似文献   
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Attirampakkam, an open-air stratified Palaeolithic site in southeastern India is the focus of ongoing studies to investigate the nature of Lower and Middle Palaeolithic occupation in relation to changing Pleistocene environments. The paucity of faunal or palaeobotanical remains at the site required the use of rock magnetic properties (χlf, χfd, χfd %, χARM, SIRM, χARM/SIRM, SIRM/χlf, χARM/χlf, χARM/χfd, S-ratio, HIRM and HIRM/IRM300mT) as proxies for deciphering the palaeoenvironments and palaeoclimates of the region. Rock magnetic data from stratified deposits within excavated trenches show that the bulk of the sedimentation was intermittent with no subaerial exposure of sediments for long periods, and points to fluctuating wetter and drier climates associated with the Acheulian to Late Middle Palaeolithic levels. There is a general trend towards a wetter climate from Layer 5 upwards. Layer 7 offers evidence of bacterial magnetite (χARM/χlf > 40 and χARM/χfd > 1000), suggesting the onset of micro-anaerobic environments as a result of floods. Greigite is indicated in Layer 5 (SIRM/χlf > 30 × 103 A m?1), which indicates a reducing environment. Layer 2 represents an arid climate (higher proportion of haematite and a coarser magnetic grain size). Layer 1a again is indicative of an arid climate (presence of calcrete, magnetically “hard” minerals and coarser magnetic grain size). Results indicate that the southeast coast of India experienced a mostly dry tropical climate during the Pleistocene. The detected occurrence of a few notably more arid intervals did not disrupt occupation of the site by successive groups of hominins.  相似文献   
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