Titlebook: Understanding an Orogenic Belt; Structural Evolution Ashok Kumar Dubey Book 2014 Springer International Publishing Switzerland 2014 Anisotr

咯咯笑

The Lower (Lesser) Himalaya oblique fault ramps formed during the pre-Himalayan tensional regime. The pre-Himalayan origin of the curvatures differentiates it from arcuate structures observed in other fold and thrust belts of the world. A model is proposed for arcuate geometry of the Mandi-Karsog Pluton. The Kangra recess is

Magnificent

The High Himalayamagmatic events. Both Vaikrita and Munsiari rocks represent two distinct rock assemblages and both have undergone pre-Himalayan metamorphism. A model is proposed to explain the occurrence of younger Vaikrita rocks on the thrust hanging wall and older Munsiari rocks in footwall of the Vaikrita thrust

浮雕寶石

peptic-ulcer

拍翅

The Modelluding the basic rocks and four phases of acid magmatism, is given along with distribution of volcanic rocks in the Himalaya. Distribution of significant structural features, which form the basis for the proposed model are described. These include evidence of seismicity below the plane of basal deta

vitrectomy

口訣

2197-9545 simultaneous development of folds and faults.Contains new m.The book provides a model for the structural evolution of the Himalaya with relevant background information making it easily accessible to earth scientists specializing in other areas. The book is divided into two parts: The first part des

大喘氣

Strike-Slip Faultip between folds and strike slip faults is discussed using natural example of the Jura mountains. Development of oblique fault ramps and significant criteria to distinguish between strike slip faults and oblique fault ramps are described.

恃強(qiáng)凌弱的人

The Himalayaerent dangers as well, e.g. seismicity, landslides, floods, glacial lake outburst, etc. Hence the study of Himalaya is important not only from the scientific point of view but also from the societal point of view. Tectonic sub divisions of the Himalaya are illustrated.

gregarious

The Tethys Himalayassed. Some of the normal faults are a result of gravity gliding. Formation of transverse extensional faults (e.g. Leopargial Horst) in a predominant compressional regime is explained. The latest displacement along the STDS is that of right lateral slip. Evidence for the reactivations are discussed.