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Books on the topic 'Residual anomalies and inversion'

Author: Grafiati
Published: 6 September 2023

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1

Heywood, Charles E. Isostatic residual gravity anomalies of New Mexico. U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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2

Robbins, S. L. Complete Bouguer and isostatic residual gravity maps of the Anadarko Basin, Wichita Mountains, and surrounding areas, Oklahoma, Kansas, Texas, and Colorado. U.S. G.P.O., 1992.

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3

Robbins, Stephen L. Complete Bouguer and isostatic residual gravity maps of the Anadarko Basin, Wichita Mountains, and surrounding areas, Oklahoma, Kansas, Texas, and Colorado. U.S. G.P.O., 1992.

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4

Robbins, S. L. Complete Bouguer and isostatic residual gravity maps of the Anadarko Basin, Wichita Mountains, and surrounding areas, Oklahoma, Kansas, Texas, and Colorado. U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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5

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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6

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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7

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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8

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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9

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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10

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Geological Survey, 2002.

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11

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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12

Solomon, Sean C. Inversion of gravity and bathymetry in oceanic regions for long-wavelength variations in upper mantle temperature and composition: Final report to the National Aeronautics and Space Administration on NASA grant NAGW-3036. The Administration, 1993.

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13

L, Smilde Peter, and SpringerLink (Online service), eds. Gravity Interpretation: Fundamentals and Application of Gravity Inversion and Geological Interpretation. Springer Berlin Heidelberg, 2009.

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14

Geological Survey (U.S.), ed. Principal facts for 133 gravity stations, with color maps of Bouguer and isostatic residual gravity anomalies on the Winnemucca 1p0s by 2p0s quadrangle, Nevada. U.S. Department of the Interior, U.S. Geological Survey, 1991.

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15

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. 2002.

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16

Heywood, Charles E. Estimation of alluvial-fill thickness in the Mimbres ground-water basin, New Mexico, from interpretation of isostatic residual gravity anomalies. 2002.

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17

Braga, Luiz F. S. Isostatic evolution and crustal structures of the Amazon continental margin determined by admittance analyses and inversion of gravity data. 1991.

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18

Bernstein, Judy B. An effect of residual T-to-C movement in varieties of English. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198747307.003.0007.

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This chapter examines verb-second (V2) cross-linguistically in closely related varieties of English: Older Scots, displaying general V2; present-day Appalachian English and African American English, displaying residual V2. Discontinuous subjects (analysed as instances of transitive expletives) and negative auxiliary inversion are shown to involve verb-movement to Focus in the two present-day varieties of English, unlike the general V2 found across Germanic languages, which involves TopicP. The area of overlap among V2 phenomena in the varieties of English studied is FocusP, which encodes the V
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19

Bidese, Ermenegildo, and Alessandra Tomaselli. Developing pro-drop. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198815853.003.0003.

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The syntax of Cimbrian, a Germanic heritage language, is at a peculiar developmental stage: on the one hand it has lost the V2 linear restriction, but still maintains both pronominal subject inversion and a residual root-embedded word order asymmetry; on the other, it is characterized by both ‘free’ subject inversion (VP DP) and the systematic violation of the ‘that-trace’ filter, but does not allow null subjects (NSs). This specific mixture of both V2- and pro-drop properties gives us an opportunity to revisit the traditional assumption that Germanic V2 is incompatible with full pro-drop. In
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20

Brown, Derek H. Projectivism and Phenomenal Presence. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199666416.003.0010.

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Projectivism asserts that we project subjective aspects of perception into what we experience as the world outside ourselves. It is minimally familiar from various phantom pains, afterimages, and hallucinations. Views like sense-datum theory arguably assert a more global, Strong Projectivism: all perceptual experiences involve and only involve direct awareness of projected elements. Strong Projectivism is an underappreciated variety of intentionalism. It straightforwardly explains the transparency of experience, and phenomena qualia theorists offer to avoid intentionalism, including blurry vis
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21

Dob, Daryl P., Elspeth E. Pickering, and Michael A. Gatzoulis. Moderate to complex congenital heart disease. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780198713333.003.0040.

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Children born with congenital heart disease no longer face the prospect of early death and a poor quality of life. In fact, most neonates with moderate to complex congenital heart disease have a survival rate to adulthood of over 80%. The ratio of adults to children with congenital heart disease is increasing, due to better surgical repairs, and longer survival with a better quality of life. In the Western world, there are more adults than children alive with congenital heart disease. This remarkable medical effort has allowed young women with congenital heart disease to mature to an age where
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