ODP - 100
Shakedown Cruise.
Holes:Determination of development of the Bahamas carbonate platform.
Holes:To elucidate the history of rifting, subsidence, and sedimentation on the Galacia margin and the beginning of seafloor spreading.
Holes:To study age and nature of dipping reflectors and underlying basement, history of passive margin, paleoceanographic, paleoclimatic, and evolution of flora and fauna of the Norwegian-Greenland Sea.
Holes:To study the early tectonic and paleoceanographic history of the North Atlantic and its connection to the Arctic Ocean through time.
Holes:Dedicated to establishing the first hole in zero-age crust in a well-studied portion of the Mid-Atlantic Ridge rift valley, south of the Kane fracture Zone. (With Leg 109)
Holes:To determine the timing and rate of extension and subsidence during the stretching phase as well as during the stage of oceanic crust emplacement.
Holes:For high resolution paleoclimatic studies of Neogene sediments.
Holes:Dedicated to establishing the first hole in zero-age crust in a well-studied portion of the Mid-Atlantic Ridge rift valley, south of the Kane fracture Zone. (With Leg 106)
Holes:To investigate geologic and hydrologic problems along the northern Barbados Ridge by penetrating the accretionary prism, the decollement and underthrust sediment to the oceanic crust.
Holes:To deepen and log Hole 504B; focus on coring and logging the sheeted dike complex.
Holes:Discovering the amplitude and timing of vertical tectonic movement of the Andean Continental Margin, and to date the onset and determine the response of the coastal upwelling circulation regime to tectonic and climatic forcing.
Holes:To address the formation and history of the Antarctic ice-sheets, Antarctic bottom water, oceanic planktonic production, and evolution of the Antarctic planktonic and benthic biota in the Weddell Sea.
Holes:To document the climatic, glacial, and oceanographic history of the region within the context of a more complete and detailed geochronologic framework than previously available.
Holes:To examine paleoceanograpy and stratigraphy in the tropical Indian Ocean and hotspot volcanism of the elevated plateaus and ridges scattered throughout the basin.
Holes:To determine onset and history of intraplate deformation, to characterize the lithofacies, diagenesis, and provenance of the Bengal Fan.
Holes:To explore the origin, evolution, and variablitiy of the Indian Ocean Monsoon and its effect on the oceanic environments of the western Arabian Sea and the paleoclimates of tropical Africa, Arabia, India and Asia.
Holes:To drill a deep hole in upper mantle peridotite with the aid of a hard rock guidebase and to conduct geophysical logging and other downhole measurements.
Holes:A transect, along with Leg 120, to study the Late Cretaceous to Holocene paleoclimatic history of East Antarctic, tectonic history of the Kerguelen Plateau, and the late Mesozoic rifting history of the Indian plate from Easr Antarctica.
Holes:A transect, along with Leg 119, to study the Late Cretaceous to Holocene paleoclimatic history of East Antarctic, tectonic history of the Kerguelen Plateau, and the late Mesozoic rifting history of the Indian plate from East Antarctica.
Holes:To ascertain the age, lithology, and depositional depth of sediments at Broken Ridge, and to determine pre-, syn-, and post-rift deposits.
Holes:To understand the Triassic-Jurassic rift history, the Cretaceous to Cenozoic post-breakup sedimentation and paleoenvironment and depositional sequences of the Exmouth Plateau.
Holes:To address the final stages of rifting and the formation of volcanic basement and early oceanic sediments in the Argo and Gascoyne Abyssal plains.
Holes:Luzon Strait,To focus on the age, stratigraphy, paleoceanography, and stress of the rocks in the Sulu and Celebes Seas. 124E - Dedicated to engineering development including Diamond Coring System (DCS), Navidrill (NCB), and Pressure Core Sampler (PCS).
Holes:To investigate the chemistry, timing and mechanism of emplacement of serpentinite seamounts and the tectonic history of the Izu-Bonin forearc.
Holes:To determine differental uplift/subsidence, the nature of volcanism, and chemistry of the arc-background and uplift/subsidence, stratigraphy and chemistry of sedimentation, and nature of basement in the forearc region of Izu-Bonin Arc.
Holes:To access the style and dynamics rifting of basement, to characterize the sedimentation and evolution, the age and history and magnitude and direction of the present stress field in the region.
Holes:To obtain a master Miocene to Holocene paleoceanographic section, detail of the depositional history of a failed back-arc rift and to conduct downhole multiship geophysical experiments.
Holes:To recover Jurassic sediment and oceanic crust that might be the oldest in the Pacific Ocean and possibly in the world oceans.
Holes:Recover a complete record of Neogene, Paleogene, and Late Cretaceous history, with the goal of achieving a detailed reconstruction of paleoceanography and paleoclimate.
Holes:Elucidation of the influence of pore fluid of accretionary prism, mechanical state of deformed sediments, and the fabrics and structural styles of sediments before and after accretion.
Holes:To study the influence of pore fluid and hydrogeology of the accretionary prism, the mechanical state, fabrics and structural styles of sediments before and after accretion.
Holes:To define the sedimentary response to global changes in sea level in the late Cenozoic and Quaternary, and to define the influence of paleochemistry, paleoclimate, and paleoceanography on carbonate platforms.
Holes:To study processes involved in the evolution of a island arc within the zone of influence of arc-ridge collision
Holes:To assess the nature and geologic history of the oceanic crust in the Lau Basin and Tonga Platform and to understand the processes that formed the island-arc systems on its east and west boundaries.
Holes:To prepare a seafloor site for future experiments needed to develop the Ocean Seismographic Network (OSN).
Holes:Recover complete, high resolution paleoclimatic records of the eastern equatorial Pacific Ocean.
Holes:To characterize the hydrothermal discharge and mineralization in the Juan de Fuca Ridge rift on a regional scale.
Holes:Focused on the effects of spreading-ridge subduction, the timing, rate, amplitude of vertical motion in the forearc, the seaward limit of continental crust, and the nature, petrology and chemical affinities of near trench volcanism.
Holes:To continue testing and development of engineering equipment as well as to provide scientific results from the East Pacific Rise.
Holes:To address a number of problems concerning guyot development including: timing and causes of platform drowning, timing and amplitude of sea level changes, and seamount latitude changes.
Holes:To address a number of problems concerning guyot development including: timing and causes of platform drowning, timing and amplitude of sea level changes, and seamount latitude changes.
Holes:To enhance understanding of the paleoceanography and paleoclimatology of the North Pacific Ocean.
Holes:To evaluate the role of fluid flow in the structural development of the Cascadia accretionary wedge and to determine how that flow controls the composition, distribution, concentration and flux of biogeochemical species.
Holes:To address questions concerning crustal and upper mantle processes.
Holes:To deepen Hole 504B with the main goals of penetrating into oceanic Layer 3 and determining the nature of the transition from Layer 2 to Layer 3.
Holes:The principal objective of Leg 149 was to sample the upper crust within the OCT of the Iberian Abyssal Plain to establish its nature and to test some of the predictions based on geophysical observations.
Holes:Address sea-level history recorded in siliciclastic sequences from a passive margin.
Holes:Describe basic physiography, plate tectonic, and volcanic history of the modern deep sea basin and evaluate the paleoceanographic and paleoenvironmental changes of these water masses.
Holes:To establish the development of volcanism with time and provide a spatial image of volcanism.
Holes:Kane Transform(MARK),The investigation of the mantle flow and partial melting history of the ultramafic rocks, the crystallization of the gabbros and the deformation and metamorphism attending seafloor spreading in this environment.
Holes:Recover sediments from a series of sites on the slope of Ceara Rise to develop a depth transect of samples for paleoceanographic reconstructions.
Holes:Amazon Fan
Holes:To evaluate the role of faults in fluid transport and the episodicity of fluid flow and its relationship to seismicity.
Holes:Determine the Neogene erosional history of the Canary basin and to provide insights into the links between mass sediment wasting on continental margins and climate/sea level change.
Holes:Investigate fluid flow, alteration and mineralization and associated geochemical fluxes, microbiological processes, and the subsurfaces nature of an active hydrothermal system on a slow spreading, sediment-free mid-ocean ridge.
Holes:To better understand the evolution of transform continental margins and to document changes in deep and intermediate waters passing through the eastern equatorial Atlantic.
Holes:Investigate the tectonic and paleoceanographic history of the Mediterranean Sea.
Holes:Recover sedimentary sequences in order to investigate the evolution of Northern Hemisphere climate on time scales ranging from hundreds to millions of years.
Holes:Investigate the nature of the Cretaceous/Tertiary Boundary and the influence of tropical seas on global ocean history and climate evolution; investigate early formation of the Caribbean Plate.
Holes:To address causes and effects of eustatic sea-level fluctuations and fluid flow processes in the margins of carbonate platforms.
Holes:Study the links between the evolution of North Pacific climate and the development of the California Current System and the climate links between the North Pacific and North America.
Holes:Focused on exploring the causes and consequences of ridge-flank hydrothermal circulation through observations of lateral gradients of temperature, pressure, fluid composition, and rock alteration.
Holes:Saanich Inlet,Investigation of the mechanisms of formation of massive sulfide deposits at sedimented ridges, history and diagenesis at sedimented rifts. MIDDLE VALLEY-Measure temperature gradient and sample hydrothermal, reinstrument and reseal CORK.
Holes:Determine mass- and fluid-flow paths through a constrained accretionary complex, to calculate mass and fluid balances, to understand these processes using structural data, physical and chemical properties of the sediments and pore fluids.
Holes:A - Determine the sediment, chemical, and fluid mass balances in the Barbados prism. B - Interpret the vertical structure, thermocline and water structure, climate variability, and to recover K/T and P/E boundaries, of the Blake Plateau.
Holes:To obtain a history of late Neogene paleoceanography and paleoclimate in the North Atlantic, millennial scale oscillations, the cyclicity of these oscillations and how these cycles relate to the history of Northern Hemisphere glaciation.
Holes:To study the nature of the basement of the Ocean-Continent Transition, to relate it to the problems of modes of lithospheric extension and rift-to-drift processes, and to test aspects of the models for these tectonic and igneous processes.
Holes:To focus primarily on the paleoceanographic and paleoclimatic aspects of the Benguela Current upwelling system and the upwelling area off Angola and Namibia with regard to early diagenetic processes taking place in this unique environment.
Holes:Obtain a section of layer 3 gabbros to document magmatic, hydrothermal, and tectonic processes in the lower ocean crust and to determine if the boundary between igneous crust and the depleted mantle lies above the Mohorovicic discontinuity.
Holes:To augment the biostratigraphic, biogeographic, paleoceanographic, and paleoclimatic history of the Southern Ocean during the Cenozoic, and to understand the role of the Southern Ocean in climate change in the Quaternary and late Neogene.
Holes:To extract the past 10 Ma of continental glaciation contained in the Antarctic Peninsula Pacific margin, compile an optimal history of grounded ice-volume fluctuation, and assess the main controls on sediment transport and deposition.
Holes:Determine the operational characteristics of the hammer drill, determine the viability of the hammer drill-in casing system, and to determine the maximum allowable slope for hammer drill operations.
Holes:Papua New Guinea,Characterize the composition and in situ properties (stress, temperature, physical properties, and fluid pressure) of an active low-angle normal-fault zone, and determine the vertical motion history of both the hanging wall and footwall.
Holes:Delineate the Cenozoic development of zonal water masses, the changing paleohydrography, the history of productivity and surface water mass fluctuations, and test the record of circum-Antarctic flow against the Milankovitch orbital model.
Holes:The paleoceanographic history of a carbonate-dominated, mid-latitude continental margin and adjacent basin during evolution of the Southern Ocean, the formulation of models, and determination of the Southern Ocean basin sea-level record.
Holes:Determine the chronology of Kerguelen/Broken Ridge magmatism, mineralogy and composition of mantle sources, melting processes, and magmatic evolution, evaluate the effects of LIP formation on the environment.
Holes:The long-term goals of Leg 184 are to determine the evolution and variability of the East Asian monsoon during the late Cenozoic and to improve our knowledge of the links between climate and tectonics.
Holes:To sample the upper oxidative zone of alteration of this oldest in situ oceanic crust (Hole 801C) and to provide the first complete section of sediment and a significant section of altered oceanic crust that enters this subduction zone.
Holes:Installation of a long-term geophysical observatory of the highest achievable sensitivity, Miocene and Younger Volcanic Ash Stratigraphy in the Western Pacific and subsidence History across the Continental Slope and Nature of the K Basement
Holes:The primary objective will be to locate the Indian/Pacific isotopic boundary and determine its configuration by investigating strongly interrelated geochemical, geophysical, and microbiological categories for discussion.
Holes:Antarctica,Date glacial activity in Prydz Bay and the Paleogene environment of Antarctica, link events in the East Antarctic Ice Sheet with changes in the Southern Ocean, acquire a record of ice advances to the shelf edge and interglacial deposits.
Holes:Provide data about the Indian Ocean and South Pacific paleoenvironments prior to opening (mid to late Eocene) of the Tasmanian Seaway, address the shallow-water (late Eocene) and deep-water breakthrough breakthroughs (Oligocene?)
Holes:To sample the decollement zone at critical points beneath the Nankai prism and PTZ to document the spatial variations in structure and fluid pressure to test these hypotheses of decollement formation and evolution.
Holes:Installation of a seismic observatory of the Global Seismic Network to study earth structure and upper mantle dynamics; paleomagnetic, geochemical and isotopic analyses of MORB basalts; to examine the Pacific lithosphere for microorganisms.
Holes:To determine age and duration of emplacement of the Ontag Java Plateau, the range and diversity of magmatism, the environment and style of eruption, formation and fundamental processes governing the crustal development of oceanic plateaus
Holes:Eastern Manus Basin,To delineate the subsurface volcanic architecture, the structural and hydrologic characteristics, and the deep-seated mineralization and alteration patterns of the PACMANUS hydrothermal field.
Holes:To investigate paleoceanographic variations in the western Coral Sea, to correlate these variations with changes in sea level, and to determine the absolute magnitude of the major Cenozoic sea-level falls.
Holes:Kuroshio Current,Set a long-term observatory at the summit of South Chamorro Seamount, and installation of a broadband seismometer for a long-term subseafloor borehole observatory in the Philippine Sea abyssal seafloor.
Holes:Conduct logging-while-drilling (LWD) activities at three sites previously cored on the Muroto Transect during Legs 131 and 190, Sites 808 and 1173 will be sealed with multipacker advanced circulation obviation retrofit kits (ACORKs).
Holes:To obtain cores from lava flows suitable for paleomagnetic, paleolatitude, and radiometric age determinations, and to determine the geochemical variation of the volcanic products of the Hawaiian hotspot through time.
Holes:To address the long-term climatic transition into and out of "greenhouse" climate and abrupt climatic events; to characterize changes in surface and deep waters, including vertical gradients of temperature, oxygenation, and corrosiveness.
Holes:To study the evolution of the equatorial Pacific current, provide continuous records of sea surface and abyssal temperatures, stability of the water column, heat transfer out of the tropics, ocean circulation, and trade wind belts and ITCZ.
Holes:Nuuanu Landslide,To drill one hole near the Hawaii-2 Observatory junction box to install a high-quality broadband three-component borehole seismometer (0.001-5.0 Hz) connected to the Hawaii-2 cable for power supply and continuous real-time telemetry.
Holes:To explore the distribution, activities, community structure, phylogenetic affinities, and global biogeochemical consequences of microbial communities buried in deep-sea sediments including the Peru coastal margin and Peru Basin.
Holes:The objectives are paleoceanographic: to assess climate and oceanographic changes in the southeast Pacific over Neogene time, to probe the climate system at three different but compatible scales: tectonic, orbital, and millennial.
Holes:To drill one hole in the western equatorial Pacific, to case and grout to the basement and sediments for a future (DEOS) multidisciplinary observatory. This project primarily represents the interests of the DEOS program and ION.
Holes:The igneous and alteration history of the basement on the incoming plate. Characterizing and monitoring the three hydrological systems: in basement, in the uppermost section of the subducting sediment, and the decollement and upper conduit.
Holes:Characterize the nature of magmatic accretion and the primary and secondary chemical composition, as well as the tectonic and seismic structure of the uppermost oceanic crust, establish a cased reentry hole that is open for future drilling.
Holes:To fill gaps in understanding wholesale extinctions linked to massive perturbations of the global carbon cycle and changes in the Earth's climate from the Cretaceous and Paleogene (oceanic anoxic events and Late Paleocene Thermal Maximum).
Holes:Provide a detailed history of paleoceanographic variations and characterization of depth-dependent changes in deepwater chemistry and circulation associated with episodes of early Cenozoic climate change including EECO, PETM, and EOGM.
Holes:Characterize spatial variation of mantle deformation patterns, peridotite composition, melt migration features, and hydrothermal alteration along MAR axis.
Holes:Document rifting of non-volcanic margins, including mantle unroofing, decompression melting, the origin of the deep and crustal asymmetry between conjugates, age-subsidence and strain-partitioning history, and the stratigraphic record.
Holes: