Structural and tectonic evolution of orogenic belts, with an emphasis on kinematics of shear zones, accretionary/collisional orogens and Archean tectonics

造山带的结构和构造演化，重点是剪切带、增生/碰撞造山带和太古代构造运动学

• 批准号: RGPIN-2019-04305
• 负责人: Lin, Shoufa
• 金额: $ 3.13万
• 依托单位: University of Waterloo
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2019
• 资助国家: 加拿大
• 起止时间: 2019-01-01 至 2020-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=688711
• 关键词: Structural; tectonic; evolution; orogenic; belts

*** The long term goal of my research is to develop a stronger understanding of structural and tectonic evolution of mountain belts, the evolution of tectonic processes through time, and the structural and tectonic control on mineralization. The proposed study will focus on three ancient mountain belts of contrasting ages and styles: the Proterozoic to Mesozoic South China Block and the Paleozoic Central Asian Orogenic Belt (CAOB) in China and the Archean Superior craton in Canada.*** *Continental margins, especially passive margins, commonly have irregular shapes and exhibit promontories and reentrants. Where this is the case, collision between two continents is expected to start at a promontory or between two promontories. This has major implications for tectonic evolution of orogens, but has drawn only limited attention. A better understanding of the role of irregular continental margins in collision through a study of the Early Paleozoic Orogen in South China is one of the objectives of the proposed study. Promontory collision offers a solution to the biggest puzzle concerning South China in the early Paleozoic, that is, a major tectono-thermal event in South China, with characters of a collisional orogeny, took place tens of millions of years after the Gondwana supercontinent had been assembled and collision appeared to have been over.*** *Our work in the CAOB will focus on the timing and processes of the final closure of the Paleo-Asian Ocean, through a detailed study of a Carboniferous-Permian volcano-sedimentary sequence and syntectonic intrusions and a potential ophiolite sequence. We will also pay special attention to the geometry, kinematics, temporal evolution and the tectonic significance of major terrane-bounding shear zones.*** *Our work on the Superior craton has led to the recognition of evidence for both vertical and horizontal tectonism and, more importantly, for their synchronous operation. We have proposed that synchronous vertical and horizontal tectonism was an important process in the Neoarchean and represented a transition from dominant vertical tectonism in the Meso-(and Paleo-?) Archean to dominant horizontal tectonism in the Proterozoic and Phanerozoic. We will continue to test these interpretations and their general applicability.*** *Our field-based study will be aided by numerical modelling, using a new code developed by our team that covers the time component by solving a generalized non-steady system with finite element method. The code is optimal for simulating geological processes with large deformation and for examining structural evolution in complex orogenic processes.*** *These research efforts will train at least five graduate and many more undergraduate students in structural geology and tectonics. They will gain a competitive edge from our field-based, multidisciplinary and collaborative research experience.**

*我研究的长期目标是对山带的构造和构造演化、构造过程随时间的演化以及构造和构造对成矿的控制有更深入的了解。拟议的研究将集中在三个时代和样式截然不同的古山带：元古代至中生代的南中国地块和中国的古生代中亚造山带，以及加拿大的太古宙上克拉通。*大陆边缘，特别是被动边缘，通常形状不规则，表现为海角和折返角。在这种情况下，两个大陆之间的碰撞预计将从一个海角或两个海角之间开始。这对造山带的构造演化具有重大意义，但只引起了有限的关注。通过对中国南部早古生代造山带的研究，更好地了解不规则大陆边缘在碰撞中的作用，是本研究的目的之一。海角碰撞解开了早古生代关于南中国的最大谜团，即南中国发生了一次具有碰撞造山作用特征的大型构造热事件，该事件发生在冈瓦那超大陆组装后数千万年，碰撞似乎已经结束。*我们在CAOB的工作将通过对石炭-二叠纪火山-沉积序列、同构造侵入体和潜在的蛇绿岩序列的详细研究，集中于古亚洋最终闭合的时间和过程。我们还将特别关注主要地体边界剪切带的几何学、运动学、时间演化和构造意义。*我们在超级克拉通上的工作使人们认识到垂直和水平构造作用的证据，更重要的是，它们的同步运行。我们认为，同步的垂直和水平构造作用是新太古代的一个重要过程，代表了中(古)太古代主导的垂直构造作用的转变。太古宙至元古代和显生宙占主导地位的水平构造作用。我们将继续测试这些解释及其普遍适用性。*我们的现场研究将得到数值模拟的帮助，使用我们团队开发的新程序，该程序通过用有限元方法求解广义非定常系统来涵盖时间分量。该代码最适合于模拟大变形的地质过程，以及研究复杂造山过程中的构造演化。*这些研究工作将培养至少5名构造地质学和构造学的研究生和更多的本科生。他们将从我们基于现场、多学科和协作的研究经验中获得竞争优势。**