scholarly journals Seismic investigations of the lithosphere in an amagmatic back-arc region: North Island, New Zealand

2021 ◽  
Author(s):  
◽  
Jesse-Lee Dimech
Keyword(s):  
New Zealand ◽  
Receiver Function ◽  
Large Change ◽  
Pore Fluid ◽  
Mantle Lithosphere ◽  
Seismic Reflection Data ◽  
Reflection Data ◽  
Moho Depths ◽  
Back Arc ◽  
Mantle Earthquakes

<p>New seismic constraints on crustal and upper mantle structures, kinematics, and lithospheric rheology are reported from an amagmatic back-arc region: the southwest North Island of New Zealand. Robust earthquake locations reveal a hypocentre 'downwarp' beneath the east-west trending Taranaki–Ruapehu Line. These earthquakes occur in the uppermost mantle, at depths of 30–50 km, and are distinct from shallower 8–25 km-deep earthquakes near Mt. Ruapehu in terms of focal mechanisms and principal stress directions.  A receiver function CCP stack shows that the mantle earthquakes occur beneath a large change in crustal thickness, where the Moho 'steps' from 28 to 35 km-deep and the steepest part of that step has a 20–50° dip. The mantle earthquakes are dominated by strike-slip fault movement and have a maximum compressive stress direction of NE–SW. The existence of mantle earthquakes beneath a steeply-dipping Moho step implies some sort of dynamic modication is occurring in the mantle lithosphere. One possibility to explain these features is the convective removal of the mantle lithosphere due to a Rayleigh–Taylor-type instability.  South of the Taranaki–Ruapehu Line, the Moho conversion weakens on both the receiver function CCP stack, and marine seismic reflection data under most of the Wanganui Basin (SAHKE02 and GD100 seismic lines). However, localised bright reflections at Moho depths can be seen in both near-vertical and wide-angle seismic data. Attribute analysis of near-vertical seismic reflections suggests that the rocks beneath the reflectivity are strongly-attenuating (Q ~20) with a negative velocity contrast relative to the lower crust. These observations are interpreted to be related to the presence of serpentinite (antigorite) and/or high pore fluid pressures in the mantle wedge.  The links between hydration of amagmatic back-arcs, serpentinisation and/or high pore fluid pressures, rock viscosity, and mantle instabilities are documented here for the southwest North Island of New Zealand. These associations may be applicable to other amagmatic back-arcs around the world.</p>

scholarly journals Seismic investigations of the lithosphere in an amagmatic back-arc region: North Island, New Zealand

2021 ◽  
Author(s):  
◽  
Jesse-Lee Dimech
Keyword(s):  
New Zealand ◽  
Receiver Function ◽  
Large Change ◽  
Pore Fluid ◽  
Mantle Lithosphere ◽  
Seismic Reflection Data ◽  
Reflection Data ◽  
Moho Depths ◽  
Back Arc ◽  
Mantle Earthquakes

<p>New seismic constraints on crustal and upper mantle structures, kinematics, and lithospheric rheology are reported from an amagmatic back-arc region: the southwest North Island of New Zealand. Robust earthquake locations reveal a hypocentre 'downwarp' beneath the east-west trending Taranaki–Ruapehu Line. These earthquakes occur in the uppermost mantle, at depths of 30–50 km, and are distinct from shallower 8–25 km-deep earthquakes near Mt. Ruapehu in terms of focal mechanisms and principal stress directions.  A receiver function CCP stack shows that the mantle earthquakes occur beneath a large change in crustal thickness, where the Moho 'steps' from 28 to 35 km-deep and the steepest part of that step has a 20–50° dip. The mantle earthquakes are dominated by strike-slip fault movement and have a maximum compressive stress direction of NE–SW. The existence of mantle earthquakes beneath a steeply-dipping Moho step implies some sort of dynamic modication is occurring in the mantle lithosphere. One possibility to explain these features is the convective removal of the mantle lithosphere due to a Rayleigh–Taylor-type instability.  South of the Taranaki–Ruapehu Line, the Moho conversion weakens on both the receiver function CCP stack, and marine seismic reflection data under most of the Wanganui Basin (SAHKE02 and GD100 seismic lines). However, localised bright reflections at Moho depths can be seen in both near-vertical and wide-angle seismic data. Attribute analysis of near-vertical seismic reflections suggests that the rocks beneath the reflectivity are strongly-attenuating (Q ~20) with a negative velocity contrast relative to the lower crust. These observations are interpreted to be related to the presence of serpentinite (antigorite) and/or high pore fluid pressures in the mantle wedge.  The links between hydration of amagmatic back-arcs, serpentinisation and/or high pore fluid pressures, rock viscosity, and mantle instabilities are documented here for the southwest North Island of New Zealand. These associations may be applicable to other amagmatic back-arcs around the world.</p>

Marine Terraces Reveal Complex Near-Shore Upper-Plate Faulting in the Northern Hikurangi Margin, New Zealand

2020 ◽  
Vol 110 (2) ◽  
pp. 825-849 ◽  
Author(s):  
Nicola J. Litchfield ◽  
Kate J. Clark ◽  
Ursula A. Cochran ◽  
Alan S. Palmer ◽  
Joshu Mountjoy ◽  
...  
Keyword(s):  
New Zealand ◽  
Plate Boundary ◽  
River Mouth ◽  
Seismic Reflection Data ◽  
Subduction Earthquakes ◽  
Reflection Data ◽  
Marine Terraces ◽  
Need To Evaluate ◽  
Near Shore ◽  
Recent Earthquakes

ABSTRACT Recent earthquakes involving multiple fault ruptures highlight the need to evaluate complex coastal deformation mechanisms, which are important for understanding plate boundary kinematics and seismic and tsunami hazards. We compare ages and uplift of the youngest Holocene marine terraces at Puatai Beach and Pakarae River mouth (∼10  km apart) in the northern Hikurangi subduction margin to examine whether uplift is the result of subduction earthquakes or upper-plate fault earthquakes. From stepped platform-cliff morphology, we infer uplift during 2–3 earthquakes and calculate an average uplift-per-event of 2.9±0.5  m at Puatai Beach and 2.0±0.5  m at Pakarae River mouth. Radiocarbon ages from the youngest beach deposit shells on each terrace and a tephra coverbed on one terrace constrain the timing of earthquakes to 1770–1710, 1100–910, and 420–250 cal. B.P. at Puatai Beach, and 1490–1290 and 660–530 cal. B.P. at Pakarae River mouth. The ages differ at each site indicating uplift is neither the result of subduction earthquakes nor single upper-plate fault earthquakes. A reinterpretation of new and existing bathymetry and seismic reflection data, combined with dislocation modeling, indicates that near-shore fault segmentation is more complex than previously thought and ruptures likely involve multiple upper-plate faults. Future updates of the New Zealand National Seismic Hazard Model should revise the northern Hikurangi subduction seismic sources so that rupture does not uplift Puatai Beach and Pakarae River mouth and include new near-shore upper-plate faults as multifault sources.

scholarly journals Stratigraphic and tectonic framework of Late Cretaceous and Paleogene strata of southern Aotea Basin, northwest New Zealand

2021 ◽  
Author(s):  
◽  
Callum Skinner
Keyword(s):  
New Zealand ◽  
Late Cretaceous ◽  
System Analysis ◽  
Plate Boundary ◽  
Petroleum Exploration ◽  
Tectonic Activity ◽  
Small Scale ◽  
Southern Boundary ◽  
Seismic Reflection Data ◽  
Reflection Data

<p>Seismic reflection data reveal thick sediment sequences of Late Cretaceous to Paleogene age in the region northwest of Taranaki Basin. A new stratigraphic framework for latest Cretaceous and Paleogene strata is created based on stacking patterns and stratal termination relationships of seismic reflectors. Sequence-bounding reflectors are tied to petroleum exploration wells, including recently-drilled Romney-1, to assign age and paleoenvironment interpretation. I identify the following sequences: (1) a late Haumurian to Teurian (68 – 56 Ma) aggradational shelf sequence, with at least two regressional events linked to eustatic sea-level falls; (2) a diachronous deepening of the basin that progressed from north to south during the late Waipawan to Heretaungan (53 – 46 Ma); (3) small-scale volcanism at the southern boundary with Taranaki Basin is contemporaneous with this deepening; (4) a prograding delta on Challenger Plateau during the Porangan to Runangan (46 – 35 Ma) that is evidence for tectonic uplift of the basin margins; and (5) an onlapping sequence from latest Runangan to present (35 – 0 Ma) that indicates Challenger Plateau subsided 1,300 m. A revised set of paleogeography maps and generalised stratigraphic chart summarise these observations. The Eocene phase (52-46 Ma) of tectonic subsidence and diffuse volcanism is one of the earliest signs of tectonic activity associated with development of the Cenozoic plate boundary through New Zealand. Petroleum system analysis reveals that southern Aotea Basin is prospective for petroleum exploration, with 3 plays identified in the Late Haumurian to Teurian (79 – 56 Ma) strata, in spite of Romney-1 proving unsuccessful.</p>

Identifying seismically active blind thrusts by geomorphology and seismic reflection profiles in a reactivated back-arc failed rift basin, Northeast Japan

2020 ◽  
Author(s):  
Tatsuya Ishiyama ◽  
Hiroshi Sato ◽  
Naoko Kato ◽  
Susumu Abe ◽  
Satoru Yokoi ◽  
...  
Keyword(s):  
High Resolution ◽  
Seismic Reflection ◽  
Data Depth ◽  
Alluvial Plain ◽  
The Sea Of Japan ◽  
Seismic Reflection Data ◽  
Reflection Data ◽  
Blind Thrust ◽  
Structural Growth ◽  
Back Arc

&lt;p&gt;Back-arc failed rifts in many subduction zones are recognized as mechanically and thermally weak zones that possibly play important roles in strain accommodation at later post-rift stages within the overriding plates. In case of Miocene back-arc failed rift structures in the Sea of Japan in the Eurasian-Pacific subduction system, Quaternary activity of post-rift positive inversion of normal faults are predominant, part of which are blurred by fast subsidence in alluvial plains above densified lower crust associated with mafic intrusion into rift axis. To define such active fault-related structures in alluvial plain with subtle geomorphic signatures, we collected new high-resolution seismic reflection data across the alluvial plain (Shonai plain) in Northeast Japan, where an enigmatic 1894 earthquake event (M7.0) caused devastating damages on local communities. We deployed hundreds of portable offline seismic recorders covering whole seismic lines and provided seismic shots using Vibroseis trucks at all nearby receivers, to create high-resolution, depth-converted cross sections based on seismic reflection data. Depth-converted sections to 2-3 km depth clearly illuminate pairs of west-vergent, thrust-related folds that deformed Miocene to Pleistocene sedimentary and volcaniclastic rocks. Among them, we defined previously unrecognized, west-dipping blind thrust structures beneath coastal plains that deform Pleistocene and Holocene basin-fill units. Structures of these blind thrusts are consistent with distribution of earthquake-damaged houses and, at least partly, might activate during the 1894 seismic event. Interestingly, upward extension of synclinal axial surfaces are consistent with very subtle west-facing fold scarps that deform alluvial plain deposits illuminated by DEM, suggesting recent fault activities and related structural growth of thrust-related folds. These examples nicely demonstrate that combining subtle geomorphology of constrained by DEM and high resolution seismic reflection profiling is an effective tool to define recent structural growth and activity of otherwise inaccessible blind thrust structures and mitigating their elusive seismic hazards.&lt;/p&gt;

Recent tectonic reorganization of the Nubia-Eurasia convergent boundary heading for the closure of the western Mediterranean

2011 ◽  
Vol 182 (4) ◽  
pp. 279-303 ◽  
Author(s):  
Andrea Billi ◽  
Claudio Faccenna ◽  
Olivier Bellier ◽  
Liliana Minelli ◽  
Giancarlo Neri ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Mediterranean Area ◽  
Western Mediterranean ◽  
Small Scale ◽  
The West ◽  
Seismic Reflection Data ◽  
Basin Inversion ◽  
The North ◽  
Reflection Data ◽  
Back Arc

Abstract In the western Mediterranean area, after a long period (late Paleogene-Neogene) of Nubian (W-Africa) northward subduction beneath Eurasia, subduction has almost ceased, as well as convergence accommodation in the subduction zone. With the progression of Nubia-Eurasia convergence, a tectonic reorganization is therefore necessary to accommodate future contraction. Previously-published tectonic, seismological, geodetic, tomographic, and seismic reflection data (integrated by some new GPS velocity data) are reviewed to understand the reorganization of the convergent boundary in the western Mediterranean. Between northern Morocco, to the west, and northern Sicily, to the east, contractional deformation has shifted from the former subduction zone to the margins of the two back-arc oceanic basins (Algerian-Liguro-Provençal and Tyrrhenian basins) and it is now mainly active in the south-Tyrrhenian (northern Sicily), northern Liguro-Provençal, Algerian, and Alboran (partly) margins. Onset of compression and basin inversion has propagated in a scissor-like manner from the Alboran (c. 8 Ma) to the Tyrrhenian (younger than c. 2 Ma) basins following a similar propagation of the cessation of the subduction, i.e., older to the west and younger to the east. It follows that basin inversion is rather advanced on the Algerian margin, where a new southward subduction seems to be in its very infant stage, while it has still to really start in the Tyrrhenian margin, where contraction has resumed at the rear of the fold-thrust belt and may soon invert the Marsili oceanic basin. Part of the contractional deformation may have shifted toward the north in the Liguro-Provençal basin possibly because of its weak rheological properties compared with those of the area between Tunisia and Sardinia, where no oceanic crust occurs and seismic deformation is absent or limited. The tectonic reorganization of the Nubia-Eurasia boundary in the study area is still strongly controlled by the inherited tectonic fabric and rheological attributes, which are strongly heterogeneous along the boundary. These features prevent, at present, the development of long and continuous thrust faults. In an extreme and approximate synthesis, the evolution of the western Mediterranean is inferred to follow a Wilson Cycle (at a small scale) with the following main steps : (1) northward Nubian subduction with Mediterranean back-arc extension (since ~35 Ma); (2) progressive cessation, from west to east, of Nubian main subduction (since ~15 Ma); (3) progressive onset of compression, from west to east, in the former back-arc domain and consequent basin inversion (since ~8–10 Ma); (4) possible future subduction of former back-arc basins.

scholarly journals Stratigraphic and tectonic framework of Late Cretaceous and Paleogene strata of southern Aotea Basin, northwest New Zealand

2021 ◽  
Author(s):  
◽  
Callum Skinner
Keyword(s):  
New Zealand ◽  
Late Cretaceous ◽  
System Analysis ◽  
Plate Boundary ◽  
Petroleum Exploration ◽  
Tectonic Activity ◽  
Small Scale ◽  
Southern Boundary ◽  
Seismic Reflection Data ◽  
Reflection Data

<p>Seismic reflection data reveal thick sediment sequences of Late Cretaceous to Paleogene age in the region northwest of Taranaki Basin. A new stratigraphic framework for latest Cretaceous and Paleogene strata is created based on stacking patterns and stratal termination relationships of seismic reflectors. Sequence-bounding reflectors are tied to petroleum exploration wells, including recently-drilled Romney-1, to assign age and paleoenvironment interpretation. I identify the following sequences: (1) a late Haumurian to Teurian (68 – 56 Ma) aggradational shelf sequence, with at least two regressional events linked to eustatic sea-level falls; (2) a diachronous deepening of the basin that progressed from north to south during the late Waipawan to Heretaungan (53 – 46 Ma); (3) small-scale volcanism at the southern boundary with Taranaki Basin is contemporaneous with this deepening; (4) a prograding delta on Challenger Plateau during the Porangan to Runangan (46 – 35 Ma) that is evidence for tectonic uplift of the basin margins; and (5) an onlapping sequence from latest Runangan to present (35 – 0 Ma) that indicates Challenger Plateau subsided 1,300 m. A revised set of paleogeography maps and generalised stratigraphic chart summarise these observations. The Eocene phase (52-46 Ma) of tectonic subsidence and diffuse volcanism is one of the earliest signs of tectonic activity associated with development of the Cenozoic plate boundary through New Zealand. Petroleum system analysis reveals that southern Aotea Basin is prospective for petroleum exploration, with 3 plays identified in the Late Haumurian to Teurian (79 – 56 Ma) strata, in spite of Romney-1 proving unsuccessful.</p>

Predictive Seismic Reservoir Modelling in the UK Manx Basin

1992 ◽  
Vol 10 (4-5) ◽  
pp. 321-334 ◽  
Author(s):  
C.P. Ross ◽  
S.D. Flack
Keyword(s):  
Seismic Data ◽  
Seismic Reflection ◽  
Pore Fluid ◽  
Early Triassic ◽  
Reservoir Properties ◽  
Seismic Reflection Data ◽  
Reservoir Modelling ◽  
Reflection Data ◽  
Seismic Reservoir ◽  
The Uk

Within the Manx Basin, the primary reservoir is the early Triassic Helsby sandstone. The Helsby occurs in various facies, each with its own characteristic reservoir properties. Although seismic reflection data is insensitive to changes in the pore fluid fill, geophysical modelling has shown that it should be possible to map porosity variations on conventional seismic data.

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