2003
DOI: 10.1029/2001gc000227
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PaleoMac: A Macintosh™ application for treating paleomagnetic data and making plate reconstructions

Abstract: This brief note provides an overview of a new Macintosh™ application, PaleoMac, (MacOS 8.0 or later, 15Mb RAM required) which permits rapid processing of paleomagnetic data, from the demagnetization data acquired in the laboratory, to the treatment of paleomagnetic poles, plate reconstructions, finite rotation computations on a sphere, and characterization of relative plate motions. Capabilities of PaleoMac include (1) high interactivity between the user and data displayed on screen which provides a fast and e… Show more

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Cited by 441 publications
(259 citation statements)
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“…11b) At this time, only a remnant part of the Junggar Ocean was still in subduction in the inner part of the orocline (Windley et al, 2007). The closure of the basin was accommodated by internal deformation of the orocline and by the development of strike slip faults with dextral kinematics in Tian Shan (Laurent-Charvet et al, 2002, 2003Wang et al;2007) and Kazakhstan (Samugyn, 1974) (Fig. 11d) Since Permian or Early Triassic, the Central Asia has experienced successive reactivations due to the agglomeration of Tibetan blocks and the collision India-Eurasia.…”
Section: Tentative Reconstructionmentioning
confidence: 98%
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“…11b) At this time, only a remnant part of the Junggar Ocean was still in subduction in the inner part of the orocline (Windley et al, 2007). The closure of the basin was accommodated by internal deformation of the orocline and by the development of strike slip faults with dextral kinematics in Tian Shan (Laurent-Charvet et al, 2002, 2003Wang et al;2007) and Kazakhstan (Samugyn, 1974) (Fig. 11d) Since Permian or Early Triassic, the Central Asia has experienced successive reactivations due to the agglomeration of Tibetan blocks and the collision India-Eurasia.…”
Section: Tentative Reconstructionmentioning
confidence: 98%
“…This motion was accommodated by large sinistral and dextral dextral motion in Altai and Tian Shan shear zones, respectively. As evidenced by numerous Ar-Ar dating and kinematic studies (Laurent-Charvet et al, 2002, 2003Wang et al;2007), strike-slip faulting continues in Late Permian, leading to large rotations to achieve the present configuration of Central…”
Section: Discussionmentioning
confidence: 99%
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