✦ LIBER ✦

The determinants of the voting premium in Italy: The evidence from 1974 to 2003

✍ Scribed by Lorenzo Caprio; Ettore Croci

Book ID: 116615197
Publisher: Elsevier Science
Year: 2008
Tongue: English
Weight: 223 KB
Volume: 32
Category: Article
ISSN: 0378-4266
DOI: 10.1016/j.jbankfin.2008.04.001

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Dividend privileges and the value of vot

Dividend privileges and the value of voting rights: Evidence from Italy

✍ Bigelli, Marco; Croci, Ettore 📂 Article 📅 2013 🏛 Elsevier Science 🌐 English ⚖ 316 KB

The determinants of academic outcomes in

The determinants of academic outcomes in a competing risks approach: evidence from Italy

✍ Clerici, Renata; Giraldo, Anna; Meggiolaro, Silvia 📂 Article 📅 2014 🏛 Taylor and Francis Group 🌐 English ⚖ 214 KB

The Determinants of Outsourcing and Offs

The Determinants of Outsourcing and Offshoring Strategies in Industrial Districts: Evidence from Italy

✍ Capasso, Marco; Cusmano, Lucia; Morrison, Andrea 📂 Article 📅 2013 🏛 Taylor and Francis Group 🌐 English ⚖ 253 KB

The Determinants of Motion Picture Box O

The Determinants of Motion Picture Box Office Performance: Evidence from Movies Produced in Italy

✍ M. Bagella; L. Becchetti 📂 Article 📅 1999 🏛 Springer US 🌐 English ⚖ 102 KB

Attitudes to voting rules and electoral

Attitudes to voting rules and electoral system preferences: Evidence from the 1999 and 2003 Scottish Parliament elections

✍ John Curtice; Ben Seyd 📂 Article 📅 2011 🏛 Elsevier Science 🌐 English ⚖ 238 KB

From thickening to extension in the Vari

From thickening to extension in the Variscan belt — kinematic evidence from Sardinia (Italy)

✍ P. Conti; L. Carmignani; G. Oggiano; ; 📂 Article 📅 1999 🏛 John Wiley and Sons 🌐 English ⚖ 896 KB

The Variscan nappe stack of SE Sardinia originated as a result of several stages of nappe imbrication during the Lower Carboniferous phases of the Variscan orogeny. The crustal shortening caused regional SSW‐and W‐directed thrusting, greenschist facies metamorphism and open‐to‐isoclinal polyphase fo