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STUDIES ON MEASUREMENT OF PINEAL CALCIFICATION IN PLAIN CRANIOGRAM Yoshitoki Murase 1 , Sengai Tanaka 1 , Atsuro Futamura 1 , Takao Ito 1 , Ken Imamura 1 , Kazuki Sakata 1 , T. Taketomo 1Second Department of Surgery, Gifu University School of Medicine pp.1021-1026
Published Date 1971/9/1
DOI https://doi.org/10.11477/mf.1406202966
  • Abstract
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Pineal calcification in plain craniogram is a useful landmark for estimating location of intracranial space-occupying lesions. Various methods of measur-ing its standard position hitherto have been reported. However, in applying these methods practically, inconveniences sometimes may be encountered. One of the inconveniences is that, when A-P or P-A film is made while the head happened to be some-what rotated around the vertical axis, lateral shift of pineal calcification may be difficult to be deter-mined. Another problem is that the known methods of measuring the position of pineal calcification in lateral film are relatively complicated or incon-venient. In this report we studied influence of slight head rotation on estimation of lateral shift of pineal calcification in A-P or P-A film, using craniograms of 150 normal subjects.

Study was further performed on a simple method of measuring pineal calcification in lateral film, which was devised by ourselves. The following results were obtained.

1) In normal subjects, the center of pineal cal-cification in A-P or P-A film existed within 2. 5 mm in either direction from the midpoint of the inner horizontal skull diameter passing through the pineal calcification, irrespective of slight rotation of the head around the vertical axis. Location of the calcification outside this range will be pathological.

2) In normal subjects, the center of pineal calci-fication in lateral film existed near the midpoint M of the line AL (or A0L). The line AL (or A0L) is defined as follows. The crossing point A of the curved line, indicating anterior border of the middle cranial fossa, and the line, indicating lower surface of the orbital roof, (or the midpoint A0 of the crossing point A1 and A2 on both sides) is connected by a line to outer lambda. and the point at which the inner table is crossed is named L. In most of the cases the center of pineal calcification was found to exist inside a square of 12 ×1.2 mm2, of which the center was located 4 mm anterior to and 2 mm below the point M. In cases where lambda was hardly identified, it was found that the point L could be substituted by the point L', which was a point on the inner table 10 cm distant from the most caudal point B on the inner table of the occipital bone. Location of the center of pineal calcification outside this square probably will be pathological.


Copyright © 1971, Igaku-Shoin Ltd. All rights reserved.

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電子版ISSN 2185-405X 印刷版ISSN 0006-8969 医学書院

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