Outcrops, isotopic ages, terranes and the undesirable fate of tectonic interpretations

IF 1.5 Q1 Earth and Planetary Sciences Geodinamica Acta Pub Date : 2013-12-01 DOI:10.1080/09853111.2013.858953
A. Şengör
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引用次数: 10

Abstract

This paper embodies a criticism of the recent proliferation of papers reporting high-quality isotopic ages combined with extremely poor tectonic interpretations resulting from an absence or non-consideration of high-quality geological mapping and ignorance of the basic tenets of tectonics, particularly of the comparative anatomy of mountain ranges. It appears that some geologists began to think that chronology (not even chronostratigraphy) alone is sufficient for understanding the geological history of a region. This seems a result of the mistaken belief that one kind of data can yield the clues to the entire geological history of an area. The kind of data chosen has become a matter of the most recent fashion, a sort of ‘methodomania,’ not what is required by the geological nature of the region under investigation. The appreciation that geological data are woefully incomplete and inadequate in most cases (even where superb geological maps exist) to generate perfect reconstructions is being lost. This brings with it the grave danger of impoverishing our conceptual repertoire of geological structures and evolutionary paths of tectonic entities such as orogens, taphrogens and keirogens leading to poor interpretations bereft of any sound geological basis.
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露头、同位素年龄、地形和构造解释的不良命运
本文对最近大量报道高质量同位素年龄的论文进行了批评,这些论文结合了由于缺乏或不考虑高质量地质填图以及对构造学基本原理(特别是山脉的比较解剖学)的无知而导致的极其糟糕的构造解释。似乎有些地质学家开始认为,单靠年代学(甚至不是年代学)就足以了解一个地区的地质历史。这似乎是一种错误信念的结果,即一种数据可以提供一个地区整个地质历史的线索。所选择的数据类型已经成为一种最新的时尚,一种“方法至上”,而不是被调查地区的地质性质所要求的。在大多数情况下(即使有极好的地质图),地质数据严重不完整,不足以产生完美的重建,这种认识正在消失。这带来了一个严重的危险,即使我们对地质构造和构造实体(如造山带、裂山带和造山带)的演化路径的概念库变得贫瘠,导致缺乏任何可靠地质基础的糟糕解释。
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来源期刊
Geodinamica Acta
Geodinamica Acta 地学-地球科学综合
CiteScore
4.50
自引率
0.00%
发文量
0
审稿时长
25 weeks
期刊介绍: Geodinamica Acta provides an international and interdisciplinary forum for the publication of results of recent research dealing with both internal and external geodynamics. Its aims to promote discussion between the various disciplines that work on the dynamics of the lithosphere and hydrosphere. There are no constraints over themes, provided the main thrust of the paper relates to Earth''s internal and external geodynamics. The Journal encourages the submission of papers in all fields of earth sciences, such as biostratigraphy, geochemistry, geochronology and thermochronology, geohazards and their societal impacts, geomorphology, geophysics, glaciology, igneous and metamorphic petrology, magmatism, marine geology, metamorphism, mineral-deposits and energy resources, mineralogy, orogeny, palaeoclimatology, palaeoecology, paleoceanograpgy, palaeontology, petroleum geology, sedimentology, seismology and earthquakes, stratigraphy, structural geology, surface processes, tectonics (neoteoctonic, plate tectonics, seismo-tectonics, Active tectonics) and volcanism. Geodinamica Acta publishes high quality, peer-reviewed original and timely scientific papers, comprehensive review articles on hot topics of current interest, rapid communications relating to a significant advance in the earth sciences with broad interest, and discussions of papers that have already appeared in recent issues of the journal. Book reviews are also included. Submitted papers must have international appeal and regional implications; they should present work that would be of interest to many different specialists. Geographic coverage is global and work on any part of the world is considered. The Journal also publishes thematic sets of papers on topical aspects of earth sciences or special issues of selected papers from conferences.
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