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Transpressional Regime In Asir Tectonic Terrane, Saudi Arabia

Description:

This book investigates the late Neoproterozoic N-S trending Wadi Yiba Shear Zone (WYSZ) in southern Arabian Shield. WYSZ played a significant role in the structural shaping of the basement lithologies (gneisses, metavolcanics, Ablah Group (meta-clastic and marble units) and syn- and post-tectonic granitoids) exposed in Wadi Yiba, Asir tectonic terrane. Effects of, at least, three phases of deformation are detected (D1–D3). Among these phases, D2 deformation phase was intensive and pervasive, and responsible for the formation of the WYSZ. Minor and major F2 thrust- and shear zone-related folds are coeval to this phase. The deformation patterns in the area reflect the progressive convergence between East and West Gondwanalands


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Transpressional Regime In Asir Tectonic Terrane, Saudi Arabia

Product ID: U365922555K
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AED42570

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Transpressional Regime In Asir Tectonic Terrane, Saudi Arabia

Product ID: U365922555K
Condition: New
Transpressional Regime In Asir Tectonic Terrane, Saudi Arabia-0
Type: Paperback

AED42570

Price includes VAT & Import Duties
Availability: In Stock

Quantity:

|

Order today to get by 7-14 business days

This item qualifies for free delivery

Returns & Warranty policies

Imported From: United States

At BOLO, we work hard to ensure the products you receive are new, genuine, and sourced from reputable suppliers.

BOLO is not an authorized or official retailer for most brands, nor are we affiliated with manufacturers unless specifically stated on a product page. Instead, we source verified sellers, authorized distributors or directly from the manufacturer.

Each product undergoes thorough inspection and verification at our consolidation and fulfilment centers to ensure it meets our strict authenticity and quality standards before being shipped and delivered to you.

If you ever have concerns regarding the authenticity of a product purchased from us, please contact Bolo Support. We will review your inquiry promptly and, if necessary, provide documentation verifying authenticity or offer a suitable resolution.

Your trust is our top priority, and we are committed to maintaining transparency and integrity in every transaction.

All product information, images, descriptions, and reviews originate from the manufacturer or from trusted sellers overseas. BOLO is not affiliated with, endorsed by, or an authorized retailer for most brands listed on our website unless stated otherwise.

While we strive to display accurate information, variations in packaging, labeling, instructions, or formulation may occasionally occur due to regional differences or supplier updates. For detailed or manufacturer-specific information, please contact the brand directly or reach out to BOLO Support for assistance.

Unless otherwise stated, all prices displayed on the product page include applicable taxes and import duties.

BOLO operates in accordance with the laws and regulations of United Arab Emirates. Any items found to be restricted or prohibited for sale within the UAE will be cancelled prior to shipment. We take proactive measures to ensure that only products permitted for sale in United Arab Emirates are listed on our website.

All items are shipped by air, and any products classified as “Dangerous Goods (DG)” under IATA regulations will be removed from the order and cancelled.

All orders are processed manually, and we make every effort to process them promptly once confirmed. Products cancelled due to the above reasons will be permanently removed from listings across the website.

Description:

This book investigates the late Neoproterozoic N-S trending Wadi Yiba Shear Zone (WYSZ) in southern Arabian Shield. WYSZ played a significant role in the structural shaping of the basement lithologies (gneisses, metavolcanics, Ablah Group (meta-clastic and marble units) and syn- and post-tectonic granitoids) exposed in Wadi Yiba, Asir tectonic terrane. Effects of, at least, three phases of deformation are detected (D1–D3). Among these phases, D2 deformation phase was intensive and pervasive, and responsible for the formation of the WYSZ. Minor and major F2 thrust- and shear zone-related folds are coeval to this phase. The deformation patterns in the area reflect the progressive convergence between East and West Gondwanalands


No Customer Reviews

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