中国东部大陆边缘中生代晚期增生过程的数值模拟：以那丹哈达为例

陶建丽; 楼达; 戴黎明; 李三忠; 董昊; 马芳芳; 兰浩圆; 李法坤; 王亮亮; 刘泽

doi:10.16562/j.cnki.0256-1492.2019040101

中国东部大陆边缘中生代晚期增生过程的数值模拟：以那丹哈达为例

1.
海底科学与探测技术教育部重点实验室，中国海洋大学海洋地球科学学院，青岛 266100

2.
青岛海洋科学与技术国家实验室，海洋地质过程与环境功能实验室，青岛 266237

3.
中国石油大港油田公司，天津 300280

基金项目: 国家重点研发计划项目“多板块汇聚与晚中生代成矿大爆发的深部过程”(2017YFC0601401)、“华北古陆中新元古代原型盆地及差异改造”(2016YFC0601002)；国家自然科学基金重大研究计划“西太平洋地球系统多圈层相互作用”(91858215)

详细信息

作者简介: 陶建丽(1993—)，女，硕士生，从事地球动力学数值模拟研究，E-mail：ouctaojianli@faxmail.com

通讯作者: 戴黎明(1980—)，男，副教授，从事构造地质学及其数值模拟研究，E-mail：dlming@ouc.edu.cn

中图分类号: P736.15

收稿日期: 2019-04-01

修回日期: 2019-04-16

刊出日期: 2019-10-25

Numerical simulation of Late Mesozoic accretion process along the continental margin of East China: A case study of the Nadanhada Terrane

1.
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

3.
PetroChina Dagang Oilfield Company , Tianjin 300280, China

More Information

Corresponding author: DAI Liming, dlming@ouc.edu.cn

Received Date: 01 April 2019

Revised Date: 16 April 2019

Publish Date: 25 October 2019

摘要

摘要:
许多现存造山带中均发现了洋岛玄武岩（OIB）和地幔柱型蛇绿岩记录，因此洋底高原增生是大陆生长的重要方式，但目前对控制洋底高原增生过程的机制仍不清楚。采用热-机械-岩石学模型数值模拟研究洋底高原的陆缘增生过程，结果显示洋底高原向大陆边缘增生具有3个控制因素：（1）减薄的大陆边缘；（2）海洋岩石圈中的“薄弱”层；（3）年轻的洋底高原。模拟结果与中国东北地区那丹哈达地体的野外构造解析结果和地球化学特征结合，揭示了洋底高原和东北亚大陆边缘的强烈挤压引起俯冲带的应变集中，产生与阿尔卑斯型褶皱相关的高角度逆冲断层和背冲断层，并伴随低级变质作用的构造折返过程。
- 洋底高原增生 /
- 数值模拟 /
- 构造折返 /
- 那丹哈达地体
Abstract:
Accretion of oceanic plateau is an important process of continental growth, and is exemplified by the presence of oceanic island basalts (OIB) and plume-type ophiolites in many modern orogens. Oceanic plateau can also subduct along convergent margins, as revealed by seismic tomography. The mechanism controlling accretion or subduction of oceanic plateau remain unclear. In this paper, we investigate the accretion of oceanic plateaus at continental margins using a thermo-mechanical-petrological model of an ocean-continent convergent zone. The results of the models show three major factors for the accretion of the oceanic plateaus onto the continental margin: (1) thinned continental margin for the overriding plate, (2) “weak” layers in oceanic lithosphere and (3) young oceanic plateau. The results of the model are further compared with the field structural analysis and geochemical characteristics of the Nadanhada Terrane in Northeast China. It is revealed that the intense compression of the seamount and the continental margin of Northeast Asia results in strain concentration in the subduction zone, forming high-angle thrust faults and back thrusts associated with the Alpine-type folds, and structural exhumation of low-metamorphic rocks through thrust faults.
- oceanic plateaus accretion /
- numerical modelling /
- tectonic exhumation /
- Nadanhada Terrane

HTML全文

图 1 那丹哈达及周缘地体的构造格局（根据文献[15, 20]）

Figure 1.

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图 2 初始模型和边界条件

Figure 2.

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图 3 小型洋底高原增生的构造演化过程及地形起伏（模型1正常陆缘）

Figure 3.

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图 4 小型洋底高原增生的构造演化过程及地形起伏（模型6减薄陆缘以及蛇纹石层存在）

Figure 4.

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图 5 小型洋底高原增生的构造演化过程及地形起伏（模型9减薄陆缘以及存在超铁镁质基底层）

Figure 5.

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图 6 小型洋底高原增生的构造演化过程及地形起伏（模型7减薄陆缘以及新生的小型洋底高原）

Figure 6.

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图 7 那丹哈达地体的增生样式

Figure 7.

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表 1 模型中使用的黏滞性流变参数^{[28, 31-35]}

Table 1. Thermal and visco-plastic parameters used in the numerical models^{[28, 31-35]}

岩石类型	ρ₀ /(kg·m⁻³)	Cp /(J·kg⁻¹·K⁻¹)	K /(W·m⁻¹·K⁻¹)	Hr /(μW·m⁻³)	流变性质	η₀ /(Pa·s⁻¹)	E /(kJ·mol⁻¹)	V /(J·MPa⁻¹·mol⁻¹)	n	A_D /(MPa⁻ⁿ·s⁻¹)	C /MPa	sin （φ_eff）
沉积物	2 700	1 000		2	湿石英岩	1.97E+17	154	0	2.3	3.20E-06	1	0.15
上陆壳	2 700	1 000		1	湿石英岩	1.97E+19	154	0	2.3	3.20E-06	20	0.15
下陆壳	3 000	1 000		1	斜长石 An75	4.80E+22	238	0	3.2	3.30E-04	20	0.45
洋壳/洋底高原	3 000	1 000		0.25	斜长石 An75	4.80E+22	238	0	3.3	3.30E-04	20	0.45
新生成的洋底高原	2 900	1 000		0.25	斜长石 An75	4.80E+20	238	0	3.3	3.30E-04	20	0.45
干地幔	3 300	1 000		0.022	无水橄榄岩	3.98E+16	532	8	3.5	2.50E+04	40	0.6
含水地幔	3 200	1 000		0.022	含水橄榄岩	5.01E+20	470	8	4	2.00E+03	1	0.06
蛇纹石化地幔	3 200	1 000		0.022	蛇纹石	3.21E+36	8.9	3.2	3.8	1.97E-33	1	0.06
基性岩浆底侵作用	3 200	1 000		3	单斜辉石	3.21E+36	670	0	2.7	1.56E-34	1	0.06
注：ρ₀为参考密度；C_p为比热容；k为导热系数；Hr为放射性热；C为内聚力；sin（φ_eff）为有效摩擦系数；η₀为参考黏滞参数；E为活化能；V为活化体积；n为应力指数；A_D为材料常数。

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表 2 模型中部分熔融岩石的流变学参数^{[27, 31, 33]}

Table 2. Parameters of partially molten rocks in the numerical models^{[27, 31, 33]}

部分熔融岩石类型	ρ₀ /(kg·m⁻³)	Cp /(J· kg⁻¹·K⁻¹)	sin （φ_eff）	η₀ /(Pa·s⁻¹)	T_固相线 /K	T_液相线 /K	H_L /(kJ·kg⁻¹)	n	A_D /(MPa⁻ⁿ·s⁻¹)
部分熔融沉积物/上陆壳	2 500	1 500	0.06	5.00E+14		831+0.06P	300	1	2.00E-09
部分熔融下陆壳	2 500	1 500	0.06	5.00E+14		1,423+0.105P	300	1	2.00E-09
部分熔融洋壳/洋底高原	2 900	1 500	0.06	1.00E+13		1,423+0.105P	300	1	1.00E-07
注：ρ₀为熔融岩石的参考密度；C_p为熔融岩石的比热容；sin（φ_eff）为熔融岩石的有效摩擦系数；η₀为熔融岩石的有效摩擦系数；T_固相线为地壳的固相线温度；T_液相线为地壳的液相线温度；H_L为相变潜热；n为熔融岩石的应力指数；A_D为熔融岩石的材料常数。

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表 3 模型条件设置

Table 3. Description of the numerical models used in this work

模型编号	减薄大陆边缘	蛇纹石化地幔	超铁镁质层基底	年轻的洋底高原	是否增生
1						图 3
2	√
3		√
4				√
5		√		√
6	√	√			√	图 4
7	√			√	√	图 2(a), 图 6
8			√
9	√		√		√	图 5
注：√ 代表符合条件。

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中国东部大陆边缘中生代晚期增生过程的数值模拟：以那丹哈达为例

1. 海底科学与探测技术教育部重点实验室，中国海洋大学海洋地球科学学院，青岛 266100 2. 青岛海洋科学与技术国家实验室，海洋地质过程与环境功能实验室，青岛 266237 3. 中国石油大港油田公司，天津 300280

作者简介: 陶建丽(1993—)，女，硕士生，从事地球动力学数值模拟研究，E-mail：ouctaojianli@faxmail.com

通讯作者: 戴黎明(1980—)，男，副教授，从事构造地质学及其数值模拟研究，E-mail：dlming@ouc.edu.cn

Numerical simulation of Late Mesozoic accretion process along the continental margin of East China: A case study of the Nadanhada Terrane

Corresponding author: DAI Liming, dlming@ouc.edu.cn

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1.
海底科学与探测技术教育部重点实验室，中国海洋大学海洋地球科学学院，青岛 266100

2.
青岛海洋科学与技术国家实验室，海洋地质过程与环境功能实验室，青岛 266237

3.
中国石油大港油田公司，天津 300280