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JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact support@jstor.org.. The Econometric Society is collaborating with JSTOR to digitize, preserve and extend access to Econometrica.Exact expressions are given for the first two moments of a linear combination of the elements of an instrumental variables estimator for the coefficients of the endogenous variables in a general structural equation. These results generalize previous exact results for equations containing just two or three endogenous variables. In addition, we provide bounds on the moments that can easily be estimated, and generalize some earlier qualitative results for these estimators. 'The results reported in this paper are extensions of the results in the two earlier papers [9 and 18]. We are grateful to Professor Takeshi Amemiya and a referee for suggesting the collaboration that led to the final version of the paper. The authors would like to thank A. W. Davis for valuable technical advice, and Yasuko Chikuse for supplying the reference [3] which corrects some earlier formulae in [2].

Twenty-four cases of dengue haemorrhagic fever/dengue shock syndrome were studied in Delhi in the months of September and October, 1988. The majority of these cases were boys aged 6-10 years. Classical symptoms of dengue (fever, headache, aesthesia, myalgia) occurred in all the patients. Digestive symptoms (nausea, vomiting, anorexia, abdominal pain and hepatomegaly) were also common. Haemorrhagic manifestations were present in 41.7% of the cases. Of these, 90% had gastrointestinal haemorrhages. Shock occurred in 17 cases (70.8%). Thrombocytopenia and prolongation of coagulation profile were found in 62.5% of cases. Three patients (12.5%) who presented with encephalopathy died. The other 21 patients recovered after an average period of 2-8 days.

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Five hundred and forty four cases of cerebral palsy were studied to find the etiology. Male to female ratio was 1.9:1. Prenatal, natal and postnatal factors were found in 42 (7.72%), 238 (43.75%) and 142 (26.1%) cases respectively. Only 79 (14.52%) cases were found to have more than one factor which could have contributed to brain damage. In 43 (7.9%) cases the prenatal, natal and postnatal history were normal and the cause was not known. Toxemia (1.29%) cases and microcephaly (1.84%) cases were the most common etiological factors in the prenatal category. Among the natal causes, birth anoxia was the most common etiological factor and was observed in 24.45% cases. Infections of the central nervous system comprised the major etiopathogenetic factors of the postnatal causes--11.95% cases had encephalitis, while 5.15% cases had meningitis. In cases where more than one etiology was present, the most frequent causes were a combination of prematurity or birth anoxia in association with toxemia, antepartum hemorrhage, prolonged labour, twins, forceps or caesarean delivery. Anoxia was consistently the most common etiological factor in those cases of monoplegia paraplegia, quadriplegia, diplegia, and ataxia, i.e. in 0.55%, 1.29%, 11.76%, 6.07% and 0.55% cases respectively. The present study reveals that majority of the cases were found to have natal or post natal etiology.

In the present study, some naphthalene derivatives have been synthesized by incorporating azetidinyl and thiazolidinyl moieties at its alpha- or beta-positions such as alpha-(3-chloro-2-oxo-4-substituted)aryl-1-azetidinyl)naphthalenes 6-10, alpha-((substituted)aryl-4-oxo-1,3-thiazolidin-3-yl)naphthalenes 11-15, beta-(3-chloro-2-oxo-4-substituted aryl-1-azetidinyl)naphthalenes 21-25, and beta-(substituted aryl-4-oxo-1,3-thiazolidin-3-yl)naphthalenes 26-30. These compounds have also been screened for acute toxicity and anti-inflammatory and analgesic activities. Compounds which showed better anti-inflammatory and analgesic activities were also examined for their ulcerogenic liability and underwent a cyclooxygenase assay. Two compounds, 12 and 28, were found to exhibit potent anti-inflammatory activity as compared to the standard drugs phenylbutazone and naproxen.

The middle Eocene Fulra Limestone Formation of the Kachchh Basin, western India was investigated to interpret depositional environments and sources of limestones based on facies analysis, mineralogy, and major, trace, and rare earth elements (REEs) geochemistry. Facies stacking pattern of the Fulra Limestone Formation exhibits an overall shallowing-upward sedimentary succession developed in the middle to inner ramp to lagoonal set-up. Staining of the thin sections and X-ray diffraction patterns show dominance of calcite mineral. The CaO, ranging from 40.45% to 49.69%, is the dominant oxide among the major oxides followed by SiO 2 (4.04-10.3%). The dominance of CaO over MgO suggests that the major mineral phase has been calcite and no dolomitization occurred during the deposition of the Fulra limestone. The low proportion of SiO 2 and Al 2 O 3 suggests low siliciclastic input during the precipitation of the Fulra limestone that is confirmed by the positive correlation of ∑REE with Al 2 O 3 , Fe 2 O 3 , Ni, Th, Sc, and Y and the negative correlation of SiO 2 , Al 2 O 3 , and Sr with CaO. The average value of REE contents in the Fulra Limestone Formation are lower (*16.02 ppm) than the average value of typical marine carbonates (*28 ppm). The Post-Archean Australian Shale-normalized REE + Y patterns of the Fulra limestone exhibit seawater like shale-normalized REE + Y pattern, whereas slightly lower average value of Y/Ho ratio (34.60) than the typical seawater value (~44-74) suggests modification of the seawater, to some extent, by input of freshwater in a coastal environment. The REEs of the Fulra Limestone Formation have similarity with the carbonates of the Arabian Sea and/or shallow marine carbonates with exception of a few elements. It is envisaged from this study that the Fulra limestone was deposited in a shallow marine to coastal set-up where mixing of the continental material in seawater was feasible.