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左侧岩下窦逆行血流及海绵窦盗血与中央静脉狭窄相关:磁共振血管造影表现

Retrograde flow in the left inferior petrosal sinus and blood steal of the cavernous sinus associated with central vein stenosis: MR angiographic findings.

作者信息

Paksoy Yahya, Genç Bülent Oğuz, Genç Emine

机构信息

Ultra Görüntüleme Merkezi (Imaging Center), Konya, Turkey.

出版信息

AJNR Am J Neuroradiol. 2003 Aug;24(7):1364-8.

Abstract

BACKGROUND AND PURPOSE

We attempted to identify the cause of abnormal venous flow seen during arterial MR angiography in the inferior petrosal sinus by use of in three female patients (aged 51, 48, and 70 years, respectively).

METHODS

Arterial 3D time-of-flight MR angiography was performed with a tilted optimized nonsaturating excitation pulse sequence (TR/TE, 31/7; flip angle, 20 degrees; section thickness, 65 mm; effective thickness, 1 mm; number of sections, 1 to 2); no magnetization transfer pulse sequence was used. Contrast-enhanced 3D MR angiography of the neck was performed with a 3D fast low-angle shot pulse sequence (TR/TE, 4.6/1.8; flip angle, 40 to 45 degrees; section thickness, 80 mm; intersection gap, 1.5 mm; acquisition matrix, 180 x 256; acquisition time, 27 s) on a system with a whole-body coil.

RESULTS

In all three patients, 3D time-of-flight MR angiography revealed abnormal vascular signal originating from the left cavernous sinus, continuing through the inferior petrosal sinus, and ending in the proximal internal jugular vein at the jugular bulb level. Abnormal vascular signal at the jugular bulb, sluggish flow and flow-related enhancement in the left internal jugular vein, and signal void in the contralateral jugular vein were noted. Contrast-enhanced delayed-phase MR angiography showed stenosis in the left brachiocephalic vein in all patients.

CONCLUSION

High signal intensity noted at the inferior petrosal sinus resulted from retrograde flow. Retrograde flow was due to blood stealing from the internal jugular vein toward the cavernous sinus because of venous stenosis in the brachiocephalic vein.

摘要

背景与目的

我们试图通过对3例女性患者(年龄分别为51岁、48岁和70岁)进行研究,来确定在岩下窦动脉磁共振血管造影(MR angiography)过程中所观察到的异常静脉血流的原因。

方法

采用倾斜优化非饱和激励脉冲序列(TR/TE,31/7;翻转角,20°;层厚,65mm;有效层厚,1mm;层数,1至2)进行动脉三维时间飞跃法MR血管造影;未使用磁化传递脉冲序列。在配备全身线圈的系统上,采用三维快速低角度激发脉冲序列(TR/TE,4.6/1.8;翻转角,40至45°;层厚,80mm;层间距,1.5mm;采集矩阵,180×256;采集时间,27s)进行颈部对比增强三维MR血管造影。

结果

在所有3例患者中,三维时间飞跃法MR血管造影均显示异常血管信号起源于左侧海绵窦,经岩下窦延续,在颈静脉球水平终止于颈内静脉近端。可见颈静脉球处异常血管信号、左侧颈内静脉血流缓慢及血流相关强化,以及对侧颈静脉内信号缺失。对比增强延迟期MR血管造影显示所有患者左侧头臂静脉均有狭窄。

结论

岩下窦处的高信号强度是由逆流所致。逆流是由于头臂静脉狭窄导致血液从颈内静脉盗血至海绵窦。

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