塔宁巴尔海槽断裂特征与构造演化

doi:10.11867/j.issn.1001-8166.2021.046

地球科学进展 ›› 2022, Vol. 37 ›› Issue (3): 290 -302. doi: 10.11867/j.issn.1001-8166.2021.046

“东南亚构造、沉积与资源环境效应”专辑上一篇下一篇

塔宁巴尔海槽断裂特征与构造演化

何明勇 ¹ ^, ² ^, ³(

), 栾锡武 ¹(

), 魏新元 ³ ^, ⁴, 冉伟民 ² ^, ³, 穆敬轩 ¹ ^, ³, 叶传红 ¹ ^, ³, 刘洁 ³, 陈建宏 ¹ ^, ² ^, ³

^1.山东科技大学地球科学与工程学院，山东青岛 266590
^2.中国地质调查局青岛海洋地质研究所，山东青岛 266237
^3.青岛海洋科学与技术试点国家实验室，海洋矿产资源评价与探测技术功能实验室，山东青岛 266237
^4.中国海洋大学海洋地球科学学院，山东青岛 266100

收稿日期:2021-05-29 修回日期:2021-10-29 出版日期:2022-03-10
通讯作者: 栾锡武 E-mail:841804750@qq.com;xluan@sdust.edu.cn
基金资助:
中国—东盟海上合作基金项目“中国—东盟海洋地震数据平台与研究中心建设”(12120100500017001);国家自然科学基金项目“孟加拉湾东北部沉积过程与特提斯东段构造变形耦合关系”(92055211)

Fault Characteristics and Tectonic Evolution of the Tanimbar Trough

Mingyong HE ¹ ^, ² ^, ³( ), Xiwu LUAN ¹( ), Xinyuan WEI ³ ^, ⁴, Weimin RAN ² ^, ³, Jingxuan MU ¹ ^, ³, Chuanhong YE ¹ ^, ³, Jie LIU ³, Jianhong CHEN ¹ ^, ² ^, ³

^1.College of Earth Science and Engineering，Shandong University of Science and Technology，Qingdao 266590，China
^2.Qingdao Institute of Marine Geology，China Geological Survey，Qingdao 266237，China
^3.Laboratory of Marine Mineral Resources，Pilot National Laboratory for Marine Science and Technology （Qingdao），Qingdao 266237，China
^4.College of Marine Geosciences，Ocean University of China，Qingdao 266100，China

Received:2021-05-29 Revised:2021-10-29 Online:2022-03-10 Published:2022-04-14
Contact: Xiwu LUAN E-mail:841804750@qq.com;xluan@sdust.edu.cn
About author:HE Mingyong (1995-), male, Benxi City, Liaoning Province, Master student. Research areas include seismic interpretation, tectonic evolution of continental margin. E-mail: 841804750@qq.com
Supported by:
the China-ASEAN Maritime Cooperation Fund Project "China-ASEAN Marine seismic data center"(12120100500017001);The National Natural Science Foundation of China "Coupling relationship between sedimentary process and tectonic deformation of northeastern Bay of Bengal, an Eastern Tethys section"(92055211)

全文 ( 24 ) 下载PDF ( 382 )

塔宁巴尔海槽位于印度尼西亚班达弧的东南部，与帝汶海槽以及阿鲁海槽相连接。形成于澳大利亚大陆与班达弧的碰撞过程中，在弧—陆碰撞中，碰撞的轨迹、年龄和方式仍然存在争议，对于塔宁巴尔海槽是否为俯冲带也存在着争议。依据二维地震测线，运用生长指数与古落差法定量分析塔宁巴尔海槽断层，结合测井以及物源研究探讨塔宁巴尔海槽的断裂特征及其构造演化。研究结果表明，塔宁巴尔海槽在白垩世与早上新世断裂活动较为活跃，与构造活动发生的时间相一致，中生代的裂谷作用形成中生代的正断层，早上新世澳大利亚板块与班达弧发生碰撞，弧—陆碰撞导致塔宁巴尔群岛的隆升与塔宁巴尔海槽的沉降并引发了中生代断裂的再活化。海槽的变形持续至晚上新世，形成现今塔宁巴尔海槽形态。

关键词: 塔宁巴尔海槽, 弧—陆碰撞, 断裂特征, 构造演化

The Tanimbar Trough is located southeast of the Banda Arc in Indonesia， and is connected with the Timor and Aru troughs， which were formed during the collision between the Australian continent and Banda Arc. During the arc-continent collision， the track， age， and mode of collision remain controversial. It is also controversial whether the Tanimbar Trough is a subduction zone. Based on the 2D seismic lines， the growth index， and the paleo-fall method， the faults in the study area were quantitatively analyzed. Combined with logging and provenance studies， the fault characteristics and tectonic evolution of the Tanimbar Trough are discussed. The results show that the fault activity in the study area was active during the Cretaceous and Early Pliocene， which coincided with the period of tectonic activity. Mesozoic rifting formed normal Mesozoic faults， and the Australian Plate collided with the Banda Arc in the early Pliocene. The arc-land collision led to the uplift of Tanimbar Island and the subsidence of the Tanimbar Trough and triggered the reactivation of Mesozoic faults. The deformation of the trough continued until the Late Pliocene， forming the Tanimbar Trough.

Key words: Tanimbal Trough, Arc-continent collision, Fracture characteristics, Tectonic evolution

中图分类号:

P736.1

图1 塔宁巴尔海槽位置与区域构造

Fig. 1 Location and regional structure of Tanimbar Trough

图2 塔宁巴尔海槽及附近地层^{［

25
］}

Fig. 2 Tanimbar Trough and its adjacent strata^{［

25
］}

图3 二维地震测线与研究区断裂分布（位置见图1黄色线框）

Fig. 3 2D seismic lines and fault distribution in the study area （see Fig. 1 yellow box for location）

图4 断裂组合（剖面位置见图3）

Fig. 4 Fracture combination diagram （see Fig. 3 for profile location）

图5 塔宁巴尔海槽剖面（剖面位置见图3）

Fig. 5 Profile of Tanimbar Trough （see Fig. 3 for location）

图6 塔宁巴尔海槽F1~F8断层生长指数与落差定量分析

Fig. 6 Quantitative analysis of growth index and fall of fault F1~F8 in Taninbar Trough

图7 塔宁巴尔海槽F4和F6生长指数与落差分析

Fig. 7 Growth index and fall analysis of F4 and F6 in Tanimbar Trough

图8 塔宁巴尔海槽新近纪地层划分（剖面位置见图3）

Fig. 8 Stratigraphic division of Neogene in Tanimbar Trough （see Fig. 3 for the location of the section）

图9 晚白垩世至今塔宁巴尔区域沉积演化^{［

18
］}

Fig. 9 Sedimentary evolution of tanimbar area from Late Cretaceous to present^{［

18
］}

图10 塔宁巴尔海槽底部（剖面位置见图3）

Fig. 10 Bottom of Tanimbar Trough （see Fig. 3 for the location of the section）

图11 塔宁巴尔海槽构造演化^{［

11
，

26
，

47
，

50
］}

Fig. 11 Tectonic evolution map of Taninbar Trough^{［

11
，

26
，

47
，

50
］}

32	冉伟民，栾锡武，邵珠福，等. 东海陆架盆地南部生长断层活动特征［J］.海洋地质与第四纪地质， 2019， 39（1）：100-112.
33	ZHANG Hao， LUAN Xiwu， RAN Weimin， et al. Characteristics and genesis of faults in Wenchang A sag， western Pearl River Mouth Basin［J］. Marine Geology & Quaternary Geology， 2020，40（4）：96-106.
	张豪，栾锡武，冉伟民，等. 珠江口盆地西部文昌A凹陷断裂特征与成因探讨［J］.海洋地质与第四纪地质， 2020，40（4）：96-106.
34	ANONYMOUS T C. The petroleum potential of the Indonesian Banda Arc［J］. AAPG Bulletin， 2004， 88（5）：565-585.
35	PATTILLO J， NICHOLLS P J. A tectonostratigraphic framework for the vulcan graben， Timor Sea region［J］. The Appea Journal， 1990， 30（1）：27-51.
36	METCALFE I. Gondwana dispersion， Asian accretion and evolution of Eastern Tethys［J］. Australian Journal of Earth Sciences， 1996， 43（6）：605-623.
37	KATILI J A. Review of past and present geotectonic concepts of eastern indonesia［J］. Netherlands Journal of Sea Research， 1989， 24（2/3）：103-129.
38	YANG X M， ELDERS C. The Mesozoic structural evolution of the Gorgon Platform， North Carnarvon Basin， Australia［J］. Australian Journal of Earth Sciences， 2016， 63（6）：755-770.
39	LI H， WANG Y， ZHU W， et al. Seismic characteristics and processes of the Plio-Quaternary unidirectionally migrating channels and contourites in the northern slope of the South China Sea［J］. Marine & Petroleum Geology， 2013， 43：370-380.
40	JEAN F， STOW D A V， IMBERT P， et al. Seismic features diagnostic of contourite drifts［J］. Marine Geology， 1999， 162（1）：1-38.
41	BRADSHAW M T， YEATES A N， BEYNON R M， et al. Palaeogeographic eolution of the North West Shelf region［C］// Proceedings of the North West Shelf symposium. Canberra： Petroleum Exploration Society of Australia， 1988.
42	BRADSHAW J， NICOLL R S， BRADSHAW M. The cambrian to permo-Triassic Arafura Basin， Northern Australia［J］. The APPEA Journal， 1990， 30： 107-118.
43	MCLENNAN J M， RASIDI J S， HOLMES R L， et al. The geology and petroleum potential of the western Arafura Sea［J］. The APPEA Journal， 1990， 30（1）：91.
44	ROLLET N， LOGAN G A， RYAN G， et al. Shallow gas and fluid migration in the northern Arafura Sea （offshore Northern Australia）［J］. Marine & Petroleum Geology， 2009， 26（1）：129-147.
45	FATWA A， OHARA M， SAPUTRA A， et al. 3D Seismic geomorphology interpretation of Cenozoic carbonate succession in offshore Tanimbar region， Eastern Indonesia［C］// Proceedings of the indonesian petroleum association. Jakarta： INPEX Corporation， 2016.
46	CHARLTON T R， MEMD S， SAMODRA H， et al. The stratigraphic and structural evolution of the Tanimbar islands， eastern Indonesia［J］. Journal of Southeast Asian Earth Sciences， 1991， 6（3/4）：343-358.
47	KANEKO Y， MARUYAMA S， KADARUSMAN A， et al. On-going orogeny in the outer-arc of the Timor-Tanimbar region， eastern Indonesia［J］. Gondwana Research， 2007， 11（1/2）：218-233.
48	CHARLTON T R. The petroleum potential of inversion anticlines in the Banda Arc［J］. AAPG Bulletin， 2004， 88（5）：565-585.
49	KATILI J A. Tectonic evolution of eastern Indonesia and its bearing on the occurrence of hydrocarbons［J］. Marine & Petroleum Geology， 1991， 8（1）：70-83.
50	LI Sanzhong， XU Shan， ZHAO Shujuan， et al. Tectonic transition and plate reconstructions of the east Asian continental main［J］. Marine Geology & Quaternary Geology，2013，33（3）： 65-94.
	李三忠，余珊，赵淑娟，等.东亚大陆边缘的板块重建与构造转换［J］.海洋地质与第四纪地质，2013，33（3）：65-94.
51	LI Sanzhong， CAO Xianzhi， WANG Guangzeng， et al. Meso-Cenozic tectonic evolution and plate reconstruction of the Pacific Plate［J］. Journal of Geomechanics，2019，25（5）： 642-677.
1	HALL R， PATRIA A， ADHITAMA R， et al. Seram， the Seram Trough， the Aru Trough， the Tanimbar Trough and the Weber Deep： a new look at major structures in the Eastern Banda Arc［C］// Proceedings of the indonesian petroleum association. Jakarta： INPEX Corporation， 2017.
2	ROBERTS G. East Indonesia： plays and prospectivity of the West Aru， Kai Besar and Tanimbar area-identified from new long offset seismic data［C］// AAPG annual convention and exhibition. Houston， Texas， USA： AAPG， 2011.
3	CROSTELLA A. Geosynclines and plate tectonics in Banda arcs， eastern Indonesia［J］. AAPG Bulletin， 1977， 61：2 063-2 081.
4	HAMILTON W B. Tectonics of the Indonesian region［J］. Bulletin of the Geological Society of Malaysia， 1979， 6：3-10.
5	MCAFFREY R. Active tectonics of the eastern Sunda and Banda arcs［J］. Journal of Geophysical Research Solid Earth，1988， 93（B12）. DOI：10.1029/JB093iB12p15163 .
6	AUDLEY M G. Ocean trench blocked and obliterated by Banda forearc collision with Australian proximal continental slope［J］. Tectonophysics， 2004， 389（1/2）：65-79.
7	BOWIN C， PURDY G M， JOHNSTON C， et al. Arccontinent collision in Banda Sea region［J］. Electricity Journal， 1980， 15（2）：37-46.
8	SPAKMAN W， HALL R. Surface deformation and slab-mantle interaction during Banda Arc subduction rollback［J］. Nature Geoscience， 2010， 3（8）：562-566.
9	HALL R. Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean［J］. Tectonophysics， 2012， 570/571（11）：1-41.
10	HONTHAAS C， REHAULT J P， MAURY R C， et al. A Neogene back-arc origin for the Banda Sea basins： geochemical and geochronological constraints from the Banda ridges （East Indonesia）［J］. Tectonophysics， 1998， 298（4）：297-317.
11	SAQAB M， BOURGET J， TROTTER J， et al. New constraints on the timing of flexural deformation along the northern Australian margin： implications for arc-continent collision and the development of the Timor Trough［J］. Tectonophysics： International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth， 2017. DOI：10.1016/j.tecto.2016.12.020 .
12	BORCH C. Continent-Island arc collision in the Banda Arc［J］. Tectonophysics， 1979， 54（3/4）：169-193.
13	ROOSMAWATI N， HARRIS R. Surface uplift history of the incipient Banda arc-continent collision： geology and synorogenic foraminifera of Rote and Savu Islands， Indonesia［J］. Tectonophysics， 2009， 479（1/2）：95-110.
51	李三忠，曹现志，王光增，等.太平洋板块中—新生代构造演化及板块重建［J］.地质力学学报，2019，25（5）：642-677.
52	PAIRAULT A A， HALL R， ELDERS C F. Structural styles and tectonic evolution of the Seram Trough， Indonesia［J］. Marine & Petroleum Geology， 2003， 20（10）：1 141-1 160.
53	HALL R. Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific： computer-based reconstructions， model and animations［J］. Journal of Asian Earth Sciences， 2002， 20（4）：353-431.
14	AUDLEY M G. Timor-Tanimbar Trough： the foreland basin of the evolving Banda Orogen［M］. New Jersey： Blackwell Publishing Limited， 2009.
15	CHARLTON T R， SMET M， SAMODRA H， et al. The stratigraphic and structural evolution of the Tanimbar islands， eastern Indonesia［J］. Journal of Southeast Asian Earth Sciences， 1991， 6（3/4）：343-358.
16	OHARA M， NAKAMURA K， SASAKI Y. The structural evolution of Babar Selaru region in the Southern Banda Outer Arc， Eastern Indonesia［C］// Proceedings of the indonesian petroleum association， 39th annual convention and exhibition. Jakarta： INPEX Corporation， 2015.
17	METCALFE I. Gondwana dispersion and Asian accretion： tectonic and palaeogeographic evolution of eastern Tethys［J］. Journal of Asian Earth Sciences， 2013， 66（8）：1-33.
18	SAPUTRA A， OHARA M. Basin and petroleum system modeling of offshore Tanimbar region： implications of structural development history［C］// Proceedings of the indonesian petroleum association fortieth annual convention & exhibition. Jakarta： INPEX Corporation， 2016.
19	FITRIANNUR M R. New insights into the development of the Timor-Tanimbar Trough based on 3D seismic data［C］// Proceedings of the South East Asia petroleum exploration society conference. Singapore： SEAPEX， 2015.
20	CORNEE J， VILLENEURE M， REHAULT J P， et al. Stratigraphic succession of the Australian margin between Kai and Aru islands （Arafura Sea， eastern Indonesia） interpreted from Banda Sea II cruise dredge samples［J］. Journal of Asian Earth Sciences，1997. DOI：10.1016/S0743-9547（97）00026-3 .
21	BARBER A J， TJOKROSAPOETRO S， CHARLTON T R， et al. Mud volcanoes， shale diapirs， wrench faults， and melanges in accretionary complexes， Eastern Indonesia［J］. Bulletin， 1986. DOI：10.1306/94886CA9-1704-11D7-8645000102C1865D .
22	MARYONO A， HARRISON R L， COOKE D R， et al. Tectonics and geology of porphyry Cu-Au deposits along the eastern Sunda magmatic arc， Indonesia［J］. Economic Geology， 2018， 113（1）：7-38.
23	CHARLTON T R， KAYE S J， SAMODRA H S， et al. Geology of the Kai Islands： implications for the evolution of the Aru trough and Weber Basin， Banda Arc， Indoesia［J］. Marine & Petroleum Geology， 1991，8：62-69.
24	REHAULT J P， MALOD J A， VILLENEUVE M， et al. Structural framework and tectonic evolution of the Banda Sea Basins （East Indonesia）［C］// Geosea' 95. Manila. The Philippines， 1995.
25	PERDANA L A， OHARA M， SAPUTRA A， et al. Neogene hydrocarbon prospectivity of the frontier offshore Tanimbar Region in the Southern Banda Outer Arc， Eastern Indonesia［C］//Proceedings of the indonesian petroleum association. Jakarta： INPEX Corporation， 2016.
26	ZIMMERMANN S， ROBERT H. Provenance of Cretaceous sandstones in the Banda Arc and their tectonic significance［J］. Gondwana Research， 2019， 67：1-20.
27	WEI Xinyuan， LUAN Xiwu， RAN Weimin， et al. Fault characteristics and tectonic evolution model of East Timor trough［J］. Geological Bulletin of China， 2021，40（2/3）：364-375.
	魏新元，栾锡武，冉伟民，等. 东帝汶海槽断裂特征与构造演化模式［J］. 地质通报， 2021，40（2/3）：364-375.
28	LEI Baohua. Review of methods with quantitative studies of activity intensity of the growth fault［J］. Advances in Earth Science， 2012， 27（9）：947-956.
	雷宝华. 生长断层活动强度定量研究的主要方法评述［J］. 地球科学进展，2012，27（9）：947-956.
29	LIU Yuhu， CAO Chunhui， LI Ruilei， et al. The control of the spatial and temporal differential evolution of Boundary Faults on Faulted Basins—taking the Fulongquan Fault Depression in the Southern Songliao Basin as an example［J］.Advances in Earth Science， 2020， 35（1）：79-87.
	刘玉虎，曹春辉，李瑞磊等. 边界断裂时空差异演化对断陷盆地的控制作用——以松辽盆地南部伏龙泉断陷为例［J］. 地球科学进展，2020，35（1）：79-87.
30	ZHANG Zhongpei， WANG Qingchen. The summary and comment on fault-slip analysis and palaeostress reconstruction［J］. Advances in Earth Science， 2004，19（4）：605-613.
	张仲培，王清晨. 断层滑动分析与古应力恢复研究综述［J］.地球科学进展，2004，19（4）：605-613.
31	PERDANA L A， OHARA M， SAPUTRA A， et al. Neogene to Quaternary structural evolution in the Offshore Tanimbar Region in the Southern Banda Outer Arc： implications for petroleum system in Eastern Indonesia［C］// Proceedings of the indonesian petroleum association. Jakarta： INPEX Corporation， 2016.
32	RAN Weimin， LUAN Xiwu， SHAO Zhufu， et al. Active characteristics of growing faults in the south of East China Sea Shelf Basin［J］. Marine Geology & Quaternary Geology， 2019， 39（1）：100-112.

[1]	杨丽华, 刘池洋, 代双和, 周义军, 毕明波, 刘永涛. 鄂尔多斯盆地古峰庄地区断裂特征及油气地质意义[J]. 地球科学进展, 2021, 36(10): 1039-1051.
[2]	田自强, 王勇生, 胡召齐, 白桥. 大别造山带内部变沉积岩锆石LA-ICP MS U-Pb定年及其大地构造意义[J]. 地球科学进展, 2018, 33(9): 945-957.
[3]	王佳, 谭先锋, 曾春林, 陈青, 冉天, 薛伟伟, 李霞, 陈岑. 泥质岩成岩系统过程及其对SiO ₂赋存状态的制约——以渝东南地区龙马溪组为例[J]. 地球科学进展, 2017, 32(3): 292-306.
[4]	石学法，鄢全树. 西太平洋典型边缘海盆的岩浆活动[J]. 地球科学进展, 2013, 28(7): 737-750.
[5]	朱志敏,闫剑飞,沈冰,周家云. 从“构造热事件”分析阜新盆地多能源矿产共存成藏[J]. 地球科学进展, 2007, 22(5): 468-489.
[6]	王登红;邹天人;徐志刚;余金杰;付小方. 伟晶岩矿床示踪造山过程的研究进展[J]. 地球科学进展, 2004, 19(4): 614-620.
[7]	宋述光. 北祁连山俯冲杂岩带的构造演化[J]. 地球科学进展, 1997, 12(4): 351-365.

阅读次数

全文

摘要