{"title":"List of Reviewers for Volume 49","authors":"","doi":"10.1002/gj.2621","DOIUrl":null,"url":null,"abstract":"thawing of relations with Iran between 2003 and 2006. Leturmy and Robin commence their volume with an introduction that adequately sets the scene for the subsequent technical papers. Eight of these are structurally focussed, with the last five being related to stratigraphic and petroleum geological issues. In a brief review, such as this, I have chosen to mention just a few of these papers. Hatzfeld et al. outline recent advances in understanding the kinematics of the Zagros Mountains by use of GPS and Quaternary geological features, notably with reference to the Kaizerun Fault Zone, showing that deformation includes both basement and cover sediments. Regard et al. detail the structural and stratigraphical lateral transition between the Zagros orogenic belt and the Makran accretionary prism/trench subduction zone complex. A right-lateral motion is identified in which the Makran is thrust over the Zagros, along a crustal plane that dips to the NE. Navabpour et al. outline the evidence for Mesozoic extensional brittle tectonics in Interior Fars, of particular relevance when combined with an appreciation of palaeogeographic evolution of the same interval. Aubourg et al. present new magnetic fabric data from the Fars province that relate to the Neogene compression of the Zagros margin. They identify, in addition to the Late Miocene– Pliocene event, an earlier Early Miocene age event where many structures were initiated. Emami et al. examine the regional structure of the Mountain Front Flexure in Lurestan, notably the S-shaped Pusht-e-Kuh Arc with constituent Anaran anticline and its subvertical forelimb. They identify a significant collapse of the anticline with development of deep and narrow half-graben within the fold belt system. Robin et al. focus on the Mesozoic deepwater carbonates from the southern Tethyan passive margin. This contains a detailed synthesis of data from radiolarian assemblages, in addition to comprehensive logging of outcrop stratigraphy and integration","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"49 6","pages":"660"},"PeriodicalIF":2.2000,"publicationDate":"2014-11-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/gj.2621","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geological Journal","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/gj.2621","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
thawing of relations with Iran between 2003 and 2006. Leturmy and Robin commence their volume with an introduction that adequately sets the scene for the subsequent technical papers. Eight of these are structurally focussed, with the last five being related to stratigraphic and petroleum geological issues. In a brief review, such as this, I have chosen to mention just a few of these papers. Hatzfeld et al. outline recent advances in understanding the kinematics of the Zagros Mountains by use of GPS and Quaternary geological features, notably with reference to the Kaizerun Fault Zone, showing that deformation includes both basement and cover sediments. Regard et al. detail the structural and stratigraphical lateral transition between the Zagros orogenic belt and the Makran accretionary prism/trench subduction zone complex. A right-lateral motion is identified in which the Makran is thrust over the Zagros, along a crustal plane that dips to the NE. Navabpour et al. outline the evidence for Mesozoic extensional brittle tectonics in Interior Fars, of particular relevance when combined with an appreciation of palaeogeographic evolution of the same interval. Aubourg et al. present new magnetic fabric data from the Fars province that relate to the Neogene compression of the Zagros margin. They identify, in addition to the Late Miocene– Pliocene event, an earlier Early Miocene age event where many structures were initiated. Emami et al. examine the regional structure of the Mountain Front Flexure in Lurestan, notably the S-shaped Pusht-e-Kuh Arc with constituent Anaran anticline and its subvertical forelimb. They identify a significant collapse of the anticline with development of deep and narrow half-graben within the fold belt system. Robin et al. focus on the Mesozoic deepwater carbonates from the southern Tethyan passive margin. This contains a detailed synthesis of data from radiolarian assemblages, in addition to comprehensive logging of outcrop stratigraphy and integration
期刊介绍:
In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited.
The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.