摘要
近10年来,福建省基础地质调查研究工作取得重大进展,梳理总结主要有6个方面:(1)古元古代麻源岩群等结晶基底组成物质具多样性,是由不同时代、不同成因的变质杂岩组成("麻源变质杂岩");(2)造山带混杂岩填图方法将新元古代马面山(岩)群解体为"基质"和"岩块",提出"晚古生代马面山俯冲增生杂岩"认识;(3)加里东期构造活动对前泥盆纪基底影响(改造)深远而又强烈,加东期变形-变质-深熔及岩浆作用具有一致性;(4)应用锆石定年,在闽西南及闽北地区确认大量印支期(中-晚三叠世)花岗质岩体;(5)应用紫金山、马坑、上房等矿集区研究资料,构建了精细的晚中生代成矿系列与岩浆序列(四期);(6)确定了长乐—南澳构造岩浆带岩石组合、形成时代,精确划分4个造山阶段(对应四期构造-岩浆演化),反演了地壳隆升过程与机制。福建省所处特殊的地理和构造位置,是研究华南地质的关键窗口,在古老岩石和物质组成、新元古代-早古生代构造演化、晚古生代构造-岩浆热事件、中生代造山作用机制、中-新生代构造域转换、地壳生长与循环再造等一系列重大问题研究方面有独特的优势。
In the past ten years,great progress has been made in the basic geological investigation and research in Fujian Province,and there are six main aspects in combing and summing up:(1)The composition of crystalline basement of Paleoproterozoic igneous group is diverse,is composed of metamorphic complex of different ages( " ma-yuan metamorphic complex").(2)The mapping method of melange rocks in orogenic belts disintegrates the Neoproterozoic Mamianshan(rock)group into " matrix" and " rock block",and puts forward the understanding of " late Paleozoic Maomanshan subduction and accretive complex".(3)The Caledonian tectonic activity affected the pre Devonian basement(transformation)profoundly and strongly,and the eastern Canadian deformation metamorphism and deep penetration is consistent with magmatism.(4)Using zircon dating,a large number of Indosinian(Middlelate Triassic)granitic intrusions were confirmed in southwestern Fujian and northern Fujian.(5)The fine late Mesozoic metallogenic series and magmatic series(stage 4)were constructed by using the data of Zijinshan,Makeng and Shangfang ore concentration areas.(6)The rock assemblage of the Changle-Nanao tectonic magmatic belt was determined and its forming age was determined.Four orogenic stages(corresponding to the four stages of tectonicmagmatic evolution)were accurately divided into four orogenic stages and the crustal uplift process and mechanism were inversed.The special geographical and tectonic location of Fujian Province is the key window to study the geology of South China.In ancient rock and material composition,Neoproterozoic early Paleozoic tectonic evolution,late Paleozoic tectonic-magmatic thermal event,Mesozoic orogenic mechanism,The Meso-Cenozoic tectonic domain transformation,crustal growth and recycling have unique advantages in a series of important problems.
引文
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