Early Eocene Radiolarian Fauna from the Sangdanlin, Southern Tibet: Constraints on the Timing of Initial India-Asia Collision

This is a new report on the early Eocene radiolarian fauna from the Sangdanlin section in the Gyirong region, along the southern margin of the Yarlung Zangbo Suture Zone. The Sangdanlin section measured in this study is divided into three lithostratigraphic units from bottom to top： the Zongzhuo, Sangdanlin, and Zheya formations. Abundant radiolarian fossils were obtained from the Sangdanlin section and 54 species of 30 genera were identified and assigned as follows： Cryptamphorella conara-C. macropora the late Cretaceous Zone and Amphis_phaera coronate, Bur）ella tetradica-Bekoma campechensis, and B.bidartensis-B. divaricata the Paleocene-early Eocene Interval Zones. The Paleocene- early Eocene radiolarian zones are comparable to the radiolarian zones RP4-RP8 in New Zealand. Based on the data of radiolaria and lithofacies, it is suggested that the Zongzhuo Formation should be deposited along the base of the north-facing, continental slope of the Greater Indian continental margin, and the Sangdanlin Formation should be a deep marine, sedimentary sequence located in a foreland basin. The early Eocene radiolarian fauna in the Sangdanlin Formation constrains the initial age of the India-Asia collision to no later than 53.6 Ma.

Paleomagnetism of late Cretaceous dykes in the Gangdese belt: New constraints on the position and structure of the southern margin of Asia prior to the India-Asia collision

This paper report paleomagnetic data from late Cretaceous diorite dykes that sub-vertically intrude granodiorites in the eastern Gangdese belt near the city of Lhasa.Our research goals are to provide further constraints on pre-collisional structure of the southern margin of Asia and the onset of the India-Asia collision.Magnetite is identified as the main magnetic carrier in our study.The magnetite shows no evidence of metamorphism or alteration as determined from optical and scanning electron microscope observations.A strong mineral orientation is revealed by anisotropy of magnetic susceptibility analysis both for the intruded dykes and the country rocks.The authors interpret this AMS fabric to have formed during intrusion rather than deformation.Fifteen of 23 sites yield acceptable site mean characteristic remanences with dual polarities.A scatter analysis of the virtual geomagnetic poles suggests that the mean result adequately averaged paleosecular variation.The paleomagnetic pole from the Gangdese dykes yields a paleolatitude of 14.3°N±5.8°N for the southern margin of Asia near Lhasa.The paleolatitude corresponds to an in-between position of the Lhasa terrane during about 130‒60 Ma.Furthermore,the mean declination of the characteristic remanent magnetization reveals a significant counterclockwise rotation of 18°±9°for the sampling location since about 83 Ma.In the light of tectonic setting of the dykes,the strike of the southern margin of Asia near Lhasa is restored to trend approximately about 310°,which is compatible with the hypothesis that the southern margin of Eurasia had a quasi-linear structure prior to its collision with India.

Structural Relationships along a Neoarchean Arc-Continent Collision Zone, North China Craton

The Archean North China Craton is composed of the Western Block,Eastern Block and the intervening Central Orogenic Belt.A 4-10 km wide and 85 km long tectonic mélange belt informally called the Zanhuang tectonic

Numerical Modeling of Basin-Range Tectonics Related to Continent-Continent Collision

Continent-continent collision is the most important driving mechanism for the occurrence of various geological processes in the continental lithosphere. How to recognize and determine continent-continent collision, especially its four-dimensional temporal-spatial evolution, is a subject that geological communities have long been concerned about and studied. Continent-continent collision is mainly manifested by strong underthrusting (subduction) of the underlying block along an intracontinental subduction zone and continuous obduction (thrusting propagation) of the overlying block along the intracontinental subduction zone, the occurrence of a basin-range tectonic framework in a direction perpendicular to the subduction zone and the flexure and disruption of the Moho. On the basis of numerical modeling, the authors discuss in detail the couplings between various amounts and rates of displacement caused by basin subsidence, mountain uplift and Moho updoming and downflexure during obduction (thrusting propagation) and subduction and the migration pattern of basin centers. They are probably indications or criteria for judgment or determination of continent-continent collision.

On Continent-Continent Point-Collision and Ultrahigh-Pressure Metamorphism

Up to now it is known that almost all ultrahigh-pressure (UHP) metamorphism of non-impact origin occurred in continent-continent collisional orogenic belt, as has been evidenced by many outcrops in the eastern hemisphere. UHP metamorphic rocks are represented by coesite- and diamond-bearing eclogites and eclogite facies metamorphic rocks formed at 650-800℃ and 2.6-3.5 GPa, and most of the protoliths of UHP rocks are volcanic-sedimentary sequences of continental crust. From these it may be deduced that deep subduction of continental crust may have occurred. However, UHP rocks are exposed on the surface or occur near the surface now, which implies that they have been exhumed from great depths. The mechanism of deep subduction of continental crust and subsequent exhumation has been a hot topic of the research on continental dynamics, but there are divergent views. The focus of the dispute is how deep continental crust is subducted so that UHP rocks can be formed and what mechanism causes it to be subducted to great depths and again exhumed to the shallow surface. Through an analysis of the continental process and mechanical boundary conditions of the Dabie collisional belt-an UHP metamorphic belt where the largest area of UHP rocks in the world is exposed, this paper discusses the variations of viscous stresses and average pressure in the viscous fluid caused by tectonism with rock physical properties and the contribution of the tectonic stresses to production of UHP. Calculation indicates that the anomalous stress state on the irregular boundary of a continental block may give rise to stress concentration and accumulation at local places (where the compressional stress may be 5-9 times higher than those in their surroundings). The tectonic stresses may account for 20-35% of the total UHP. So we may infer that the HP (nigh-pressure)-UHP rocks in the Dabie Mountains were formed at depths of 60-80 km. Thus the authors propose a new genetic model of UHP rocks-the point-collision model. This model conforms to the basic principles of the mechanics and also to the geologic records and process in the Dabie orogenic belt. It can explain why UHP rocks do nol exist along the entire length of the collisional orogen but occur in some particular positions. The authors also propose that the eastern and western corners of the Himalaya collision zone are typical point-collision areas and that almost all UHP metamorphism of continental crustal rocks occurred in the two particular positions.

A Paleogeographic and Depositional Model for the Neogene Fluvial Succession, Pishin Belt, Northwest Pakistan: Effect of Post Collisional Tectonics on Sedimentation in a Peripheral Foreland Setting

Detailed facies analysis of the Neogene successions of the Pishin Belt （Katawaz Basin） has enabled documentation of successive depositional systems and paleogeographic settings of the basin formed by the collision of the northwestern continental margin of the Indian Plate and the Afghan Block. During the Early Miocene, subaerial sedimentation started after the final closure of the Katawaz Remnant Ocean. Based on detailed field data, twelve facies were recognized in Neogene successions exposed in the Pishin Belt. These facies were further organized into four facies associations i.e. channels, crevasse splay, natural levee and floodplain facies associations. Facies associations and variations provided ample evidence to recognize a number of fluvial architectural components in the succession e.g., low-sinuosity sandy braided river, mixed-load meandering, high-sinuosity meandering channels, single-story sandstone and/or conglomerate channels, lateral accretion surfaces （point bars） and alluvial fans. Neogene sedimentation in the Pishin Belt was mainly controlled by active tectonism and thrusting in response to the oblique collision of the Indian Plate with the Afghan Block of the Eurasian Plate along the Chaman-Nushki Fault. Post Miocene deformation of these formations successively caused them to contribute as an additional source terrain for the younger formations.

Structural and Geochronological Evidence for Multiple Episodes of Tertiary Deformation along the Ailaoshan-Red River Shear Zone, Southeastern Asia, Since the Paleocene

Structural analyses show that the Ailaoshan-Red River shear zone （ASRRSZ） in Ailao Mountain is composed of three different deformational domains. These domains may represent three episodes of left-lateral slip experienced by the ASRRSZ. The first episode of such deformation occurred throughout the eastern high-grade belt of the ASRRSZ under a transtensional regime and produced L- type tectonites of amphibolite grade. The second episode of left-lateral slip formed high strain zones overprinting the high-grade belt. Its deformational mechanism is similar to simple shear and the deformed rocks are L-S mylonites of greenschist grade. The third episode of left-lateral slip took place chiefly in a western low-grade belt of the ASRRSZ. This deformation occurred in a transpressional regime, formed an overall structure pattern of a sinistral thrust system and produced phyllonites of low-greenschist grade. Geochronological data indicated that the three episodes of left-lateral slip happened before ～58-56 Ma, at least from ～27 Ma to 22 Ma and at ～13-12 Ma respectively. The first episode of slip in the ASRRSZ appeared to correspond to the initial collision of India and Asia at ～60 Ma. The second episode took place almost at the same time as the most intensive compression and uplift in Tibet. The latest event might represent a further eastward material flow in Tibet after ～16-13 Ma. Thus, the ASRRSZ of southeastern Asia probably experienced three main episodes of Tertiary left- lateral slip in the course of intracontinental convergence since the India-Asia collision.

Set methods of left-turn waiting zone at signalized intersection

To maximize the number of vehicles passing by the stop-line in a cycle and improve the operation efficiency of intersection in China, the settlement of left-turn lane waiting-zone is becoming prevailing. Based on conflicting-point method, the internal mechanism of left-turn flow after stopping line was analyzed through taking postposition left-turn lane waiting-zone intersection for instance. The relationship between the first left-turn vehicle and the last vehicle of previous phase passing the conflicting point was expounded. According to the time of successive arriving of two vehicle flows at conflicting-point, the reasonable layout for waiting area of left-turn vehicles was researched when the clearance index was less than O. The results suggest that the appropriate layout for waiting area of left-turning vehicles can improve the operation efficiency of intersections.

基于改进快速行进平方法的无人帆船动态避碰方法

[目的]为解决无人帆船在开阔水域的多船避碰问题,对基于改进快速行进平方(IFMS)法的局部动态避碰算法进行研究。[方法]考虑到帆船的速度不可控,将其避碰行为转化为航向控制问题,并以总势场梯度下降方向为期望避碰航向。当帆船没有碰撞危险或顺风航行时,仅通过构造时间势场来避开所有静止不规则障碍并到达目标点;而当帆船存在航行约束时,根据《国际海上避碰规则》(COLREGS)为特定会遇场景设计高斯似然函数用以动态地构建障碍势场。同时,考虑到帆船的航行死区,引入局部风势场,实现帆船动态避碰与“之”字形航行策略相结合的应用需求。[结果]结果显示,所提算法可以使无人帆船在遵守避碰规则和避免航行死区的同时,成功地在各种会遇场景下实现与其他帆船、受限机动船的避碰操作,相比原始快速行进平方(FMS)算法,逆风航行时间大大缩短,避碰航迹也更加合理、安全。[结论]所提方法符合帆船运动特性及避碰规则,在复杂环境下具有较高的安全性和鲁棒性,对无人帆船自主避障技术发展具有一定的科学价值。

非通航孔桥梁防船撞系统恒阻力装置研究

为给非通航孔桥梁防船撞系统拦截过程提供稳定持续的阻力,提出了一种利用耗能索持续协同大变形和连续破断输出稳定阻力的恒阻力装置。恒阻力装置由主绳、耗能索、破断环及其它连接件组成,与自适应浮筒、拦截网、系泊浮体等装置共同组成非通航孔桥梁自适应恒阻力船舶拦阻系统,有效拦截偏航船舶,保护非通航孔桥梁和来撞船舶的安全。通过理论分析研究该装置的阻力输出特性,建立该装置的阻力输出力学模型与计算方法,并通过拉伸破坏试验验证计算方法的准确性,进一步对影响装置阻力输出的耗能索的初始间距、长度及伸长率进行分析。结果表明:恒阻力装置能够有效地输出稳定且持续的阻力;耗能索初始间距越小,恒阻力装置阻力输出越大,阻力输出越稳定;耗能索长度或伸长率越大,恒阻力装置阻力输出越大,阻力输出越稳定。该装置已应用于力洋港大桥非通航孔区桥梁防撞中,有效地保护了大桥的安全。

基于定位、速度双误差的物流无人机碰撞概率分析

物流无人机(UAV)批量运行会存在一定的碰撞风险,为量化UAV之间在空中的碰撞概率,针对物流UAV空中运行阶段开展建模分析其碰撞风险。基于冲突区域理论,建立定位、速度双误差的UAV碰撞概率模型,分析不同夹角情况下物流UAV碰撞概率变化情况。分析识别美国联邦航空管理局官网中关于民用小型UAV的事故/事件数据中的关键风险因素。结合2万飞行小时的物流UAV故障数据建立UAV安全飞行间隔模型,给出可接受安全水平下的最短飞行间隔。探究在给定飞行间隔前提下不同航迹角以及不同风向对UAV之间碰撞概率的影响。结果表明:当物流UAV之间最短安全间隔大于90.71 m时,所有飞行场景下UAV的风险水平均在可接受范围之内。当航迹角为30、60、90°时,碰撞概率随风向变化的波动范围较小,其中,航迹夹角为90°时最稳定。而当夹角为140°时,碰撞概率的波动范围较大,UAV安全飞行对环境因素更为敏感。

复杂行星表面着陆避障增广曲率制导方法

针对复杂行星表面安全着陆问题,提出避障增广曲率制导方法。在基本曲率制导律的基础上引入障碍规避增广项。该方法利用着陆器着陆空间区域划分的思想,在障碍附近易发生碰撞区域建立膨胀预警区,基于膨胀预警区推导连续解析的障碍规避制导律,在满足几何凸轨迹状态约束的同时,考虑着陆器与障碍的相对位置关系,能够快速引导着陆器远离障碍,提高着陆器着陆过程中的安全性。仿真结果表明,该方法能够有效规避复杂行星表面的地形障碍,实现在行星表面定点软着陆,具有良好的灵活性和可靠性。

晚古生代—早中生代云南德钦白马雪山岩体演化的年代学约束及地球化学特征

为深入理解金沙江构造带的地质演化历史及其时间框架,本研究对江达—德钦—维西岩浆弧西侧的地质现象进行了系统分析,并聚焦于尼侬英云闪长岩和白马雪山花岗闪长岩的成因和时代。高精度的锆石U-Pb年代学结果表明,这两类岩石分别形成于二叠纪早期(279±2.9 Ma)和晚期(255.8±5 Ma),这为金沙江构造带的地质演化提供了新的时间框架。全岩分析表明岩体为高钾钙碱性中酸性侵入岩系列,属准铝质—过铝质岩石,富集大离子亲石元素,强烈亏损高场强元素(Nb、Ta、Ti),为典型的弧岩浆特征。该岩体与加仁及鲁甸闪长岩类岩体地球化学特征相似,岩浆来源相似,但经历了不同的岩浆演化过程。结合已发表数据,本研究表明自古生代以来,金沙江构造带可能经历了至少5期花岗质岩浆事件:347~340 Ma,292~279 Ma,261~249 Ma,237~235 Ma和232~214 Ma;尼侬英云闪长岩(279±2.9 Ma)形成于金沙江古特提洋西向俯冲消减的起始阶段,而白马雪山花岗闪长岩(255.8±1.8 Ma)可能形成于俯冲阶段结束或俯冲向碰撞的转换阶段;金沙江构造带碰撞造山发生在中三叠世而止于晚三叠世中期。这些发现为理解金沙江构造带乃至整个青藏高原东部区域的构造演化和板块动力学过程提供了新的视角和制约。

基于DEM的球磨机内介质碰撞特征研究

针对某铅锌矿选厂球磨机排矿粒度指标不理想,通过破碎统计力学进行介质配比优化,得到球磨机介质推荐补加方案Φ120 mm:Φ100 mm:Φ90 mm=50∶20∶30。使用Solidworks建立具有代表性的球磨机筒体,基于离散元方法,对现场及推荐介质配比进行仿真模拟研究。引入了惰性区面积作为评价磨矿介质方案合理的指标之一,将球磨机内惰性区域面积进行对比,得出优化后的推荐方案介质配比流动性较现场方案有一定提升,惰性区面积有所减小。将介质群运动状态、速度分布特征进行对比分析,中介质群循环中心坐标向右上方由(22.8,9.8)偏移到(24,12),表明推荐方案增加了磨机内的相对速度。通过引入不同尺寸矿石的断裂能以及数值模拟磨机内碰撞能量分析得出,大颗粒矿石的一次破碎次数基本为零,粗颗粒破碎是以研磨为主导的疲劳破碎,细颗粒破碎主要是冲击破碎。通过离散元方法模拟验证了推荐方案在各方面优于现场方案,提高了球磨机内的有效研磨面积,提高了能量的利用率,降低了能耗,证明了推荐方案优于现场方案,研究结果为选厂球磨机介质配比的优化提供了参考和指导。

The influence of Cretaceous paleolatitude variation of the Tethyan Himalaya on the India-Asia collision pattern

Identifying when, where, and how India and Asia collided is a prerequisite to better understand the evolution of the Himalayan-Tibetan Plateau. Whereas with essentially the same published paleomagnetic data, a large range of different India-Asia collision models have been proposed in the literature. Based upon the premise of a northwards-moving Indian plate during the Cretaceous times, we analyze the significant variations in relative paleolatitude produced by a nearly 90° counterclockwise(CCW)rotation of the plate itself during the Cretaceous. Interestingly, recent studies proposed a dual-collision process with a Greater India basin or post-Neo-Tethyan ocean for the India-Asia collision, mainly in the light of divergent Cretaceous paleolatitude differences of the Tethyan Himalaya between the observed values and expected ones computed from the apparent polar wander path of the Indian plate. However, we find that these varied paleolatitude differences are mainly resulted from a nearly 90° CCW rotation of a rigid/quasi-rigid Greater Indian plate during the Cretaceous. On the other hand, when the Indian craton and Tethyan Himalaya moved as two individual blocks rather than a united rigid/quasi-rigid Greater Indian plate before the India-Asia collision, current available Cretaceous paleomagnetic data permit only multiple paleogeographic solutions for the tectonic relationship between the Indian plate and the Tethyan Himalayan terrane. We therefore argue that the tectonic relationship between the Indian plate and the Tethyan Himalayan terrane cannot be uniquely constrained by current paleomagnetic data in the absence of sufficient geological evidence, and the so-called Greater India basin model is just one of the ideal scenarios.

Constraining the timing of the India-Asia continental collision by the sedimentary record

Placing precise constraints on the timing of the India-Asia continental collision is essential to understand the successive geological and geomorphological evolution of the orogenic belt as well as the uplift mechanism of the Tibetan Plateau and their effects on climate,environment and life.Based on the extensive study of the sedimentary record on both sides of the Yarlung-Zangbo suture zone in Tibet,we review here the present state of knowledge on the timing of collision onset,discuss its possible diachroneity along strike,and reconstruct the early structural and topographic evolution of the Himalayan collided range.We define continent-continent collision as the moment when the oceanic crust is completely consumed at one point where the two continental margins come into contact.We use two methods to constrain the timing of collision onset:(1) dating the provenance change from Indian to Asian recorded by deep-water turbidites near the suture zone,and(2) dating the age of unconformities on both sides of the suture zone.The first method allowed us to constrain precisely collision onset as middle Palaeocene(59±l Ma).Marine sedimentation persisted in the collisional zone for another 20-25 Ma locally in southern Tibet,and molassic-type deposition in the Indian foreland basin did not begin until another 10-15 Ma later.Available sedimentary evidence failed to firmly document any significant diachroneity of collision onset from the central Himalaya to the western Himalaya and Pakistan so far.Based on the Cenozoic stratigraphic record of the Tibetan Himalaya,four distinct stages can be identified in the early evolution of the Himalayan orogen:(1) middle Palaeocene-early Eocene earliest Eohimalayan stage(from 59 to 52 Ma):collision onset and filling of the deep-water trough along the suture zone while carbonate platform sedimentation persisted on the inner Indian margin;(2) early-middle Eocene early Eohimalayan stage(from 52 to 41 or 35 Ma):filling of intervening seaways and cessation of marine sedimentation;(3) late Eocene-Oligocene late Eohimalayan stage(from 41 to 25 Ma):huge gap in the sedimentary record both in the collision zone and in the Indian foreland;and(4) late Oligocene-early Miocene early Neohimalayan stage(from 26 to 17 Ma):rapid Himalayan growth and onset of molasse-type sedimentation in the Indian foreland basin.

Effects of Crustal Eclogitization on Plate Subduction/Collision Dynamics: Implications for India-Asia Collision

2D thermo-mechanical models are constructed to investigate the effects of oceanic and continental crustal eclogitization on plate dynamics at three successive stages of oceanic subduction, slab breakoff, and continental subduction. Crustal eclogitization directly increases the average slab density and accordingly the slab pull force, which makes the slab subduct deeply and steeply. Numerical results demonstrate that the duration time from initial continental collision to slab breakoff largely depends on the slab pull force. Specifically, eclogitization of subducted crust can greatly decrease the duration time, but increase the breakoff depth. The detachment of oceanic slab from the pro-continental lithosphere is accompanied with obvious exhumation of the subducted continental crust and a sharp uplift of the collision zone in response to the disappearance of downward drag force and the induced asthenospheric upwelling, especially under the condition of no or incomplete crustal eclogitization. During continental subduction, the slab dip angle is strongly correlated with eclogitization of subducted continental lower crust, which regulates the slab buoyancy nature. Our model results can provide several important implications for the Himalayan-Tibetan collision zone. For example, it is possible that the lateral variations in the degree of eclogitization of the subducted Indian crust might to some extent contribute to the lateral variations of subduction angle along the Himalayan orogenic belt. Moreover, the accumulation of highly radiogenic sediments and upper continental crustal materials at the active margin in combination with the strong shear heating due to continuous continental subduction together cause rising of isotherms in the accretionary wedge, which facilitate the development of crustal partial melting and metamorphism.

智能防疫消杀机器人安全性及有效性研究

目的探究消杀机器人安全性和有效性的研究方法,为消杀机器人评价方法的建立提供依据。方法通过调整障碍位置并固定推拉力计,测试消杀机器人的可识别障碍范围、盲区位置、物理碰撞力度,分析消杀机器人移动安全性;利用电气安全分析仪和耐压仪,分析消杀机器人电气安全性;利用粒度分析仪测试消杀机器人的超声雾化量、粒径分布,并根据《消毒技术规范》对物体表面的喷雾消杀效果进行评价。结果消杀机器人的3种避障方式对不同高度障碍物的识别能力差别大,且存在多个盲区,物理触边传感器可有效地对其盲区内的碰撞进行防护;消杀机器人可触及电压电流和介电强度符合GB 4793.1-2007的要求;消杀机器人的平均雾化粒径值<5μm,消杀效果受相对位置影响较大,对于与消杀机器人喷雾出口等高的物体表面消杀效果好,对较低的物体表面的消杀效果不理想。结论本文提出的安全有效性研究方法是可行的,可为建立消杀机器人评价方法提供依据。

三江造山带后碰撞断裂构造带的结构与演化:以新生代剑川—兰坪盆地为例

三江造山带作为调节印度 -欧亚板块间的碰撞及后碰撞过程的重要构造带 ,具有长期多阶段复杂演化过程。在剑川—兰坪新生代盆地发育的澜沧江断裂带、中轴断裂带和乔后断裂带是三江造山带不同时期演化的具体体现。它们在产状、组成和特点等方面有着显著的差异。构造分析表明 ,澜沧江断裂带与印度 -欧亚岩石圈板块间的早期碰撞过程密切相关 ,它制约着剑川—兰坪盆地的发育 ;乔后断裂带和中轴断裂带对于剑川—兰坪盆地具有强烈的改造作用 ,是后碰撞调解过程的结果。三江造山带对于印度 -欧亚板块间碰撞的调解过程 ,包括了水平侧向逃逸与垂向物质蠕散。在剑川—兰坪地区 ,前者表现为乔后断裂早期阶段右行走滑作用产生了大约 90km的走向错移 ,而后者形成了广布于中轴断裂内遍布的小型逆冲构造和乔后断裂西部的大量逆冲和推覆体构造。

印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程——以藏东三江地区构造演化为例

对于印度与欧亚板块的侧向碰撞带,即藏东三江地区的新生代构造分析揭示出三种不同性质的构造样式,它们形成于不同的地质时期,发育于不同的地壳层次:(1)区域规模至露头尺度上发育的具有薄皮属性的逆冲断层与推覆构造,它们广泛分布于三江地区,尤其是兰坪-思茅盆地内;(2)以红河-哀牢山断裂、澜沧江和怒江-高黎贡山断裂等为代表的区域高温型走滑韧性剪切带构造和局部发育的脆性走滑断裂构造,后者在中新生代盆地内部断裂更为发育;(3)遍布全区发育的变质核杂岩构造与地堑-半地堑盆地。区域岩浆活动性与区域构造事件的发生具有密切的时空联系。区域性递进收缩事件与走滑事件发生于碰撞过程的早期阶段,并随后伴随着早期具有岩石圈板块俯冲性质的碰撞弧高钾岩浆活动,而后期的递进伸展事件诱发了板内伸展环境中的晚期高钾岩浆活动。二者之间的碱性岩浆活动间歇期,对应着区域构造体制的转变与区域伸展作用的发生,变质核杂岩的发育与微弱的钙碱性岩浆活动是其最直接的表现。区域古地磁资料分析表明,印度-欧亚板块之间的板块相互作用、区域板块与地块的旋转以及由此所致的不同构造环境制约着各种地质事件的发生与发展。北向运动的印度板块的旋转致使三江地块在新生代演化中发生了两次规模与特点不一的地块旋转过程,即早期的大角度快速旋转和晚期的小角度慢速旋转事件。它们分别对应于早期的递进收缩变形、走滑事件和具有碰撞弧属性的碱性岩浆活动与中期的区域伸展、变质核杂岩的发育与微弱的钙碱性岩浆活动性,以及后期的递进伸展作用和晚期陆内碱性岩浆活动性。