摘要
本文对位于华北克拉通东部含有深源捕虏体(晶)中、新生代火成岩进行了详细的年代学和岩石地球化学研究,尤其是对深源捕虏体(晶)进行了矿物微区主量和痕量元素研究,讨论了不同时代火成岩的成因,尤其是岩浆源区性质及其随时间的演化。基于大量的分析测试数据,应用岩石探针技术和痕量元素与同位素地球化学示踪技术,建立了华北克拉通东部中、新生代岩石圈地幔演化模型。这对揭示华北克拉通破坏产生的时间与机制具有重要意义。
锆石LA-ICP-MS U-Pb定年和K-Ar定年结果表明,本文研究的华北克拉通东部含有深源捕虏体(晶)的中、新生代火成岩主要形成于早白垩世、晚白垩世、古近纪(包括古新世和始新世),代表性火成岩包括早白垩世鲁西费县、方城玄武岩、铁铜沟高镁闪长岩;晚白垩世辽西阜新碱锅玄武岩、辽南曲家屯玄武岩、鲁东大西庄玄武岩;古新世辽南乱石山子玄武岩和始新世菜园子玄武岩。
寄主岩和深源捕虏体(晶)的岩石地球化学及矿物微区成分研究表明,(1)早白垩世鲁西铁铜沟高镁闪长岩的原始岩浆起源于拆沉的加厚陆壳物质的部分熔融,并经历了与地幔橄榄岩的反应,而费县、方城玄武质岩浆主要起源于受拆沉陆壳物质强烈改造的富集型岩石圈地幔;(2)晚白垩世玄武质岩浆起源于整体上具有亏损性质的岩石圈地幔,但该期华北克拉通东部仍具有古老岩石圈地幔的残留,并经历了多期改造过程;(3)古近纪玄武质岩浆起源于有拆沉陆壳物质参与的岩石圈地幔;(4)中生代早期拆沉物质在经历了早白垩世部分熔融之后的残留体与亏损岩石圈地幔的混合构成了晚白垩世和古近纪玄武岩的岩浆源区。上述结果表明,中生代早期拆沉的陆壳物质是改造岩石圈地幔的主体,同时它也代表了华北克拉通破坏的起始时间和机制;早白垩世时期,拆沉物质的部分熔融以及相继出现的上涌和对上覆岩石圈地幔的交代是该期华北克拉通破坏机制的主体;晚白垩世和古近纪,华北克拉通东部岩石圈地幔经历了增生和拆沉残留物质与新增生岩石圈地幔的部分熔融。
The thesis takes the Early Cretaceous high-Mg diorites, Late Cretaceous and Paleogene basalts as well as their deep -seated xenoliths and xenocrysts in the eastern North China Craton as its research target. The formation times for these igneous rocks in the eastern North China Craton are determined using K-Ar and LA-ICP-MS zircon U-Pb dating methods. Based on the major-, trace-elements, and Sr–Nd–Pb isotopic data of these basalts and mineral chemical data from the deep-seated xenoliths and xenocrysts, the natures of their magma sources and the spatial-temporal variations are discussed for the Early Cretaceous high-Mg diorites,Late Cretaceous and Paleogene basalts in the eastern North China Craton (NCC). Taken together, the Mesozoic and Cenozoic evolution model of the lithospheric mantle in the eastern North China Craton is set up.
1 Formation times of igneous rocks borne in deep-seated xenoliths and xenocrysts in the eastern North China Craton
New dating results for the igneous rocks in the study area, together with the previous dating results, indicate that Mesozoic and Cenozoic of igneous rocks borne in deep-seated xenoliths and xenocrysts in the eastern NCC can be subdivided into four stages i.e., Early Cretaceous (119～132Ma), Late Cretaceous (73～92Ma), Paleogene (58Ma) and Eocene (36～39Ma).
The 40Ar/39Ar plateau age of biotite and LA-ICP-MS zircon U-Pb age for pyroxene-diorite from the Tietonggou intrusion are 132.82±0.5Ma and 132Ma, respectively. The K-Ar dating results for Fangcheng and Feixian basalts are 125 Ma (Zhang et al., 2002) and 119Ma, respectively. The K-Ar ages for Fuxin basalts in western Liaoning are 85Ma and 92 Ma. The K-Ar dating result for Qujiatun basalts in southern Liaoning is 82 Ma. The 40Ar/39Ar plateau age of Daxizhuang basalts in eastern Shandong is 73 Ma (Yan et al., 2003). The K-Ar dating result of Luanshishanzi basalts in southern Liaoning is 58 Ma, i.e., Paleogene, whereas K-Ar age of Caiyuanzi basalts in southern Liaoning is 36-39 Ma, i.e., Eocene.
2 Magma source and its nature for the Mesozoic and Cenozoic igneous rocks borne in deep-seated xenoliths and xenocrysts
2.1 Early Cretaceous
2.1.1 Magma source and nature of Tietonggou high-Mg diorites
Early Cretaceous Tietonggou high-Mg diorites are characterized by high Mg (Mg~#=60～66), enrichment in Na(Na_2O/K_2O=1.3～1.9)and high SiO2 contents. Geochemically, they are enriched in light rare earth elements (LREEs) and large ion lithophile elements (LILEs), and extremely depleted in high field strength elements (HFSEs) and heavy rare earth elements (HREEs), and have high initial 87Sr/86Sr ratios(0.7067～0.7071)and lowεNd(t) values (-7.82～-13.30).
The mineral chemical data and the Archean Re-depletion model ages (TRD=2.60-2.68Ga) for most peridotitic xenoliths from Tietonggou high-Mg diorites in western Shandong reveal that they could come from the ancient lithospheric mantle. However, the petrography of the xenoliths such as orthopyroxene metasomatic vein,the zoned orthopyroxene between olivine and chromite, and the existence of clinopyroxene enclosing olivine, and mineral chemical data indicate the interaction between the adakitic melt and mantle peridotite had taken place.
Combined with the enrichments in LREEs, Pb and LILEs, as well as high ISr(0.7083～0.7214), lowεNd(t) value(-0.25～-11.61)for these dunite and harzburgite xenoliths, it is suggested that the primary magma for high-Mg diorites could be derived from partial melting of delaminated lower crust, and subsequently experienced an interaction of adakitic melt with the mantle peridotite in the Early Cretaceous.
2.1.2 Magma source and nature of Fangcheng and Feixian basalts
Fangcheng and Feixian basalts, chemically, are the transitional type between alkaline and subalkaline series and are enriched in LREEs , LILEs (Sr, Ba) and extremely depleted in HFSEs (Nb, Ta, Zr, Hf), as well as exceedingly high in ISr(0.709631～0.710090)and low inεNd(t)(-13.0～-14.2).
Fangcheng and Feixian basalts contain olivine, orthopyroxene and clinopyroxene xenocrysts. Chemically, they are similar to those of the same minerals from the mantle-derived peridotite xenoliths in the Cenozoic basalts from the eastern China, implying that their primary magma could be derived from the lithospheric mantle. In addition, Fangcheng and Feixian basalts contain reversely zoned clinopyroxene xenocrysts. Their REE distribution patterns suggest that their cores are similar to those of the clinopyroxenes from the eclogitic xenoliths or pyroxenite xenoliths with cumulate textures or granulite xenoliths. There is much higher Mg~# values(Mg~# =87.0～88.9)in the mantle zones than their cores and rims(Mg~# =65.0～74.2), implying that these xenocrysts might come from the previously delaminated lower continental crust and then experienced the interaction with asthenospheric material. Taken together, these lines of evidence indicate that the primitive magma for Fangcheng and Feixian basalts could be originated from partial melting of the lithospheric mantle intensively modified by the delaminated lower continental crust. Their magma sources could be composed chiefly of garnet-bearing pyroxenite.
2.2 Magma source and nature for Late Cretaceous basalts in the eastern NCC
Late Cretaceous basalts in Fuxin western Liaoning, Qujiatun basalts in southern Liaoning and Daxizhuang basalts in eastern Shandong belong to alkaline basalt series. They are characterized by relative enrichment in LREEs and LILEs, depletion in HREEs and the lack of Eu anomalies, similar to those of oceanic island basalt. Their IS(r0.709631～0.710090)andεNd(t) values (1.61～7.55) are similar to those of the Cenozoic basalts in eastern North China, implying that their primary magma could be derived from partial melting of a depleted lithospheric mantle.
The spinel-bearing harzburgite, spinel-bearing lherzolite, amphibolite–bearing lherzolite and lherzolite xenoliths can be found in Fuxin basalts from western Liaoning, whereas Daxizhuang basalts in eastern Shandong chiefly contain spinel-bearing lherzolites. The olivine, orthopyroxene and clinopyroxene xenocrysts can be also found in them. The chemical compositions of minerals from these xenoliths and xenocrysts are similar to those of kindred minerals in the mantle-derived peridotite xenolihs from the Cenozoic basalts in eastern China. The above mentioned characteristics imply that their primary magma could be derived from partial melting of the lithospheric mantle. The olivine and clinopyroxene xenocrysts enclosed in Qujiatun basalts have similar chemical compositions to kindred minerals from the pyroxenite xenolihs in the Cenozoic basalt of eastern China.
Based on REE distribution patterns, clinopyroxenes in the mantle-derived peridotite xenolihs and xenocrysts in the Late Cretaceous basalts from western Liaoningn and eastern Shandong can be subdivided into five types:
(1) Clinopyroxenes are extremely depleted in LREEs and enriched in HREEs, which suggests that the ancient lithospheric mantle could exist and the lithospheric mantle could be modified by multi-periods partial melting events. The magma source could be free in garnet.
(2) Clinopyroxenes are extremely depleted in LREEs and HREEs, and enriched in MREE(with convex upward REE patterns), implying that an ancient lithospheric mantle modified by multiple partial melting events could exist and that the garnet could exist in magma source.
(3) Clinopyroxenes are enriched in LREEs and depleted in HREEs, suggesting that they might represent the characteristics of the primitive mantle.
(4) Clinopyroxene xenocrysts are characterized by poor in LREEs and HREEs and enriched in MREE(with convex upward REE patterns)and have much higher REE abundances than the second and third clinopyroxene xenocrysts, which may represent a newly-accretionary lithospheric mantle.
(5) Clinopyroxenes are extremely enriched in LREEs and depleted in HREEs, and have high LREE/HREE ratios, which suggests that they may represent a newly-accretionary lithospheric mantle. The decrease of isothermal plane and transformation of the asthenosphere into newly-accreted lithospheric mantle could be main reasons to result in the above-mentioned characteristics, which is also supported by high REE abundance of clinopyroxene xenocrysts.
Taken together, it is proposed that the primary magmas for the Late Cretaceous basalts from eastern North China Craton could dominantly originate from partial melting of a newly accretionary depleted lithospheric mantle, that there are relicts of ancient lithospheric mantle, and that the late Cretaceous lithospheric mantle could experience the modifications of multiple thermal events.
2.3 Magma source and nature of the Paleogene and Eocene basalts
Paleogene and Eocene basalts in southern Liaoning belong to alkaline series and are characterized by relative enrichment in LREEs,depletion in HREEs and no Eu anomalies. Geochemically, they are similar to oceanic island basalt. But, Caiyuanzi basalts are relatively enriched in Sr,Ba and depleted in Zr, Hf. The Sr-Nd isotope compositions(ISr=0.70453～0.70516,εNd(t) = 0.22～3.69)for Paleogene and Eocene basalts are similar to those of the Cenozoic basalts in eastern China. Eocene basalts in Caiyuanzi have relative high ISr(0.70473～0.70516)and lowεNd(t)(0.22～2.27),which are consistent with the characteristic of relatively enriched in Ba, Sr and depleted in Zr, Hf. These characteristics imply that crust material could be involved in the magma resource.
The Mg~# values(88～94)of olivine xenocrysts in the core from Paleogene Luanshishanzi basalt and Eocene Caiyuanzi basalt are similar to those of olivines in the mantle-derived peridotite xenolihs of the Cenozoic basalts in eastern China. Caiyuanzi basalts contain reversely zoned clinopyroxene xenocrysts. Their cores have similar chemical compositions to the clinopyroxenes from granulite xenoliths, which suggests the delaminated lower continental crust could exist in the magma sources. However, clinopyroxene xenocrysts have higher Mg~# value in the mantle zones than in the rim , indicating the existence of reaction between the delaminated lower continental crust and melt with high Mg~#. This reaction is likely to happen in asthenosphere.
Clinopyroxene xenocrysts are characterized by depletion in LREEs and HREEs and enrichment in MREE and display a convex REE patterns. Compositional variations of clinopyroxene xenocrysts from core to rim reveal a more complicated evolution history of the lithospheric mantle.
Taken together, it is proposed that the Paleogene basaltic magmas could be derived from partial melting of a depleted lithospheric mantle in general, similar to those of the Late Cretaceous basalts. But, from the late Cretaceous to Paleogene, the lithospheric mantle display an evolutional trend from depletion toward the primitive mantle. The magma sources of the Late Cretaceous and Paleogene basalts could be composed of the depleted mantle and the relict of delaminated lower continental crust (rutile+garnet) after the Early Cretaceous melting.
3 Deep processes in the lithospheric mantle
3.1 Type and nature of metasomatic events
3.1.1 A silica-rich melt (liquid) metasomatism
The orthopyroxene metasomatic vein can be found in peridotitic xenoliths from Tietonggou high-Mg diorites. Chemically, its composition is similar to one in dunites but lower Mg~# values. The existence of such metasomatic vein implies that metasomatic medium should be SiO2-rich melt (liquid).
The metasomatic vein usually consists of the orthopyroxene, phlogopite and minor plagioclase in peridotitic xenoliths from Tietonggou high-Mg diorites. The existences of orthopyroxene and plagioclase also indicate that metasomatic medium should be SiO2-rich melt (liquid). Besides, the zoning orthopyroxene occurred between chromite and olivine in peridotitic xenoliths also suggests that metasomatic medium should be SiO2-rich melt (liquid).
Main reactions are as follows:
olivine (Ol)+melt I = orthopyroxene (Opx)+melt II
olivine I (Fo=92-93)+ melt I = olivine II (Fo=85-87)+ melt II (Mg-rich)
orthopyroxene (Opx)+ melt = olivine (Ol)+ Clinopyroxene (Cpx)
spinel (Sp-Cr#=30-50)+ melt I = chromite (Chr-Cr#=65-80) + melt II (melt)
3.1.2 A carbonate-rich melt (liquid) metasomatism
Clinopyroxenes in the wehrlite xenoliths from Tietonggou high-Mg diorites are extremely enriched in LREEs, depleted in HREEs and HFSEs and relatively low Ti/Eu ratios(2177～2872), suggesting that they could be resulted from crystallization of magma. Meanwhile, it also implies that the metasomatism of an important carbonate-rich melt (liquid) might have taken place in the lithosphere mantle. The poikilitic texture(Lw9-23), metasomatic veinsof the phlogopite, dolomite, talcums and magnetites Lw8-57)in the wehrlite and dunite xenoliths further support the existence of a carbonate-rich melt (liquid) metasomatism.
3.2 Magma underplating
Olivine xenocrysts in the Paleogene Luanshishanzi basalts display circle cracks and deformation and reactive rim structures, different from the porphyritic crystals in them. Moreover, olivine xenocrysts is chemically not equilibrium with its host magma.
Late Cretaceous Qujiatun basalts contain deep-seated olivine, clinopyroxene and amphibole xenocrysts. Olivine and clinopyroxene xenocrysts in Qujiatun basalts are similar to those in the Luanshishanzi basalts.
The chemical compositions of the deep-seated xenocrysts in the Paleogene Luanshishanzi basalts and the Late Cretaceous Qujiatun basalts shows that they could come from the early mantle cumulates near the crust-mantle boundary. They represent a newly accretionary crust and imply that an important magmatic underplating event had taken place before Late Cretaceous.
3.3 Melt—Peridotite interaction
Most olivine and clinopyroxene (Cpx) xenocrysts in the Early Cretaceous, Late Cretaceous, Paleogene igneous rocks in the eastern North China Craton, display positive zonal structure (except for minor reversely zoned clinopyroxene xenocrysts), i.e., the Mg~# values gradually decreasing from core to rim. Mg~# values of their cores are similar to those of olivines and Cpx from the mantle peridotite xenoliths in the Paleozoic kimberlites and the Cenozoic basalt in NE China, whereas Mg~# values of their rims are similar to those of phenocrysts in the host basalt. Taken together with the occurrence of zonal opx and opx veins in the dunites, it is suggested that the melt—peridotite interaction widely exist in the lithospheric mantle in the eastern North China Craton.
4 Evolution of the Mesozoic and Cenozoic lithospheric mantle in eastern North China Craton
Based on the above mentioned results, the Mesozoic and Cenozoic evolution model of the lithospheric mantle in eastern North China Craton is set up.
(1) The thickening of the Early Mesozoic (T1-T2) lower continental crust in eastern North China Craton: The subduction of the Yangzi Craton beneath the North China Craton in NW direction in the early Mesozoic (T1) resulted in the thickening of the lower continental crust in eastern North China Craton and could be a geodynamic background resulting in the destruction of the North China Craton.
(2) The break-off of subducted slab and the delamination of the thickened continental lithosphere in the late Triassic—Early Jurassic(T3-J1):
Eclogites were formed during the slab subduction (YC) and the thickening of lower continental crust. High density of eclogites lead to delamination, i.e., break-off of subducted slab and delamination of the thickened continental lithosphere. The formation of monzonite-syenite association with ages of 176-225Ma from Jiazishan in erstern Shandong and Tongshi in western Shangdong should result from the delamination. Taken together, it is concluded that the break-off of the subducted slab and the delamination of the thickened lithosphere could be a major mechanism to result in the destruction of the North China Craton.
(3) The Early Cretaceous SiO2-rich melt (liquid)—peridotite interaction (K1):
In the Early Cretaceous, the subduction of the Paleo-Pacific Plate beneath the Eurasian continent could agitate in the melting of early delaminated lower continental crust. These rising adakitic melts would react with the overlying lithospheric mantle. The early Cretaceous high-Mg diorites in western Shandong could come from the intrusion of these reacted melt. Meanwhile, an EM-II lithospheric mantle formed, i.e., magma source of Fangcheng and Feixian basalts.
(4) The Late Cretaceous accretion of lithospheric mantle:
In the late Cretaceous, the decrease of geothermal gradient could result in the transformation of primary asthenosphere into the lithospheric mantle, i.e., accretion of lithospheric mantle. The newly accreted lithospheric mantle and minor relicts of ancient lithospheric mantle, together with the relicts (rutile and garnet) of delaminated eclogites after the early Cretaceous melting, make up the magma source of the Late Cretaceous and Paleogene basalts.
引文
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