Role of Heat Shock Transcriptional Factor 1 and Heat Shock Proteins in Cardiac Hypertrophy

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• 作者：Haruhiro Toko ; Tohru Minamino ; Issei Komuro
• 关键词：Jordan ; Late Ediacaran-early Cambrian ; Half-graben bounded by listric faults ; Marginal alluvial fan ; Dead sea transform
• 刊名：Trends in Cardiovascular Medicine
• 出版年：2008
• 期刊代码：253_10501738
• 类别：med
• 出版时间：April 2008
• 卷：18
• 期：3
• 页码：88-93
• 文件大小：304 K

摘要

The terrestrial Umm Ghaddah Formation of late Ediacaran-early Cambrian age was deposited in NE–SW elongated intracontinental rift system basins and sub-basins bounded by active listric half-graben faults. Basin fill consists of conglomerate facies association A, deposited in a fault-controlled transverse alluvial fan system that drained northwestward and graded laterally into sandstone facies association B, deposited by a braided river system flowing northeastward axial to the rift basin. The alluvial fan facies association was deposited by rock falls and non-cohesive debris flows of sediment gravity flow origin, and by sheetflood processes.